156-611: The Denmark expedition ( Danish : Danmark-ekspeditionen ), also known as the Denmark Expedition to Greenland's Northeast Coast and the Danmark Expedition after the ship's name , was an expedition to northeastern Greenland in 1906–1908. Despite being overshadowed by the deaths under tragic circumstances of three of the expedition's leading members ( Ludvig Mylius-Erichsen (1872–1907), Niels Peter Høeg Hagen (1877–1907), and Jørgen Brønlund (1877–1907)),
312-425: A polynya and, as the sleds tried to find a way around the open water, the first supporting party returned to Danmarkshavn. The eight dog sleds continued northwards and found remains of ancient Inuit dwellings at Eskimonaesset , in the northeastern end of Holm Land . A few days later, off Amdrup Land , a second support section of two dog sleds returned south and split. As they travelled back to Danmarkshavn, one of
468-429: A "difficult language to learn, acquire and understand", and some evidence shows that children are slower to acquire the phonological distinctions of Danish compared with other languages. The grammar is moderately inflective with strong (irregular) and weak (regular) conjugations and inflections. Nouns, adjectives, and demonstrative pronouns distinguish common and neutral gender. Like English, Danish only has remnants of
624-489: A 28-square-kilometre (11 sq mi) iceberg breaking off in 2008, and then a 260 square kilometres (100 sq mi) iceberg calving from ice shelf in August 2010. This became the largest Arctic iceberg since 1962, and amounted to a quarter of the shelf's size. In July 2012, Petermann glacier lost another major iceberg, measuring 120 square kilometres (46 sq mi), or twice the area of Manhattan . As of 2023,
780-511: A combination of high temperatures and unsuitable cloud cover led to an even larger mass melting event, which ultimately covered over 300,000 sq mi (776,996.4 km ) at its greatest extent. Predictably, 2019 set a new record of 586 Gt net mass loss. In July 2021, another record mass melting event occurred. At its peak, it covered 340,000 sq mi (880,596.0 km ), and led to daily ice losses of 88 Gt across several days. High temperatures continued in August 2021, with
936-577: A former case system , particularly in the pronouns. Unlike English, it has lost all person marking on verbs. Its word order is V2 , with the finite verb always occupying the second slot in the sentence. Danish is a Germanic language of the North Germanic branch . Other names for this group are the Nordic or Scandinavian languages. Along with Swedish, Danish descends from the Eastern dialects of
1092-509: A hypothetical future would greatly increase ice loss, but still wouldn't melt the entire ice sheet within the study period. On the ice sheet, annual temperatures are generally substantially lower than elsewhere in Greenland: about −20 °C (−4 °F) at the south dome (latitudes 63° – 65°N ) and −31 °C (−24 °F) near the center of the north dome (latitude 72°N (the fourth highest "summit" of Greenland ). On 22 December 1991,
1248-458: A kilometer with the tide. It has been suggested that if similar processes can occur at the other glaciers, then their eventual rate of mass loss could be doubled. There are several ways in which increased melting at the surface of the ice sheet can accelerate lateral retreat of outlet glaciers. Firstly, the increase in meltwater at the surface causes larger amounts to flow through the ice sheet down to bedrock via moulins . There, it lubricates
1404-526: A literary language. Also in this period, Danish began to take on the linguistic traits that differentiate it from Swedish and Norwegian, such as the stød , the voicing of many stop consonants, and the weakening of many final vowels to /e/. The first printed book in Danish dates from 1495, the Rimkrøniken ( Rhyming Chronicle ), a history book told in rhymed verses. The first complete translation of
1560-464: A marked increase in glacial earthquakes between 1993 and 2005. Since then, it has remained comparatively stable near its 2005 position, losing relatively little mass in comparison to Jakobshavn and Kangerlussuaq, although it may have eroded sufficiently to experience another rapid retreat in the near future. Meanwhile, smaller glaciers have been consistently losing mass at an accelerating rate, and later research has concluded that total glacier retreat
1716-707: A number of Danes remained as a minority within German territories . After the occupation of Denmark by Germany in World War II, the 1948 orthography reform dropped the German-influenced rule of capitalizing nouns, and introduced the letter ⟨å⟩ . Three 20th-century Danish authors have become Nobel Prize laureates in Literature : Karl Gjellerup and Henrik Pontoppidan (joint recipients in 1917) and Johannes V. Jensen (awarded 1944). With
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#17327831873521872-468: A phase of [[North Atlantic oscillation]] increasing snowfall. Every summer, a so-called snow line separates the ice sheet's surface into areas above it, where snow continues to accumulate even then, with the areas below the line where summer melting occurs. The exact position of the snow line moves around every summer, and if it moves away from some areas it covered the previous year, then those tend to experience substantially greater melt as their darker ice
2028-482: A similarity in pronunciation, combined with the long tradition of having Danish as a written language, which has led to similarities in vocabulary. Among younger Danes, Copenhageners are worse at understanding Swedish than Danes from the provinces. In general, younger Danes are not as good at understanding the neighboring languages as the young in Norway and Sweden. The Danish philologist Johannes Brøndum-Nielsen divided
2184-428: A single ice sheet first covered most of the island some 2.6 million years ago. Since then, it has both grown and contracted significantly. The oldest known ice on Greenland is about 1 million years old. Due to anthropogenic greenhouse gas emissions , the ice sheet is now the warmest it has been in the past 1000 years, and is losing ice at the fastest rate in at least the past 12,000 years. Every summer, parts of
2340-586: A so-called multiethnolect in the urban areas, an immigrant Danish variety (also known as Perkerdansk ), combining elements of different immigrant languages such as Arabic, Turkish, and Kurdish, as well as English and Danish. Within the Danish Realm , Danish is the national language of Denmark and one of two official languages of the Faroe Islands (alongside Faroese ). There is a Faroese variant of Danish known as Gøtudanskt . Until 2009, Danish
2496-560: A temperature of −69.6 °C (−93.3 °F) was recorded at an automatic weather station near the topographic summit of the Greenland Ice Sheet, making it the lowest temperature ever recorded in the Northern Hemisphere . The record went unnoticed for more than 28 years and was finally recognized in 2020. These low temperatures are in part caused by the high albedo of the ice sheet, as its bright white surface
2652-625: A variant of Standard Danish, Southern Schleswig Danish , is spoken in the area. Since 2015, Schleswig-Holstein has officially recognized Danish as a regional language , just as German is north of the border. Furthermore, Danish is one of the official languages of the European Union and one of the working languages of the Nordic Council . Under the Nordic Language Convention , Danish-speaking citizens of
2808-407: A very large vowel inventory consisting of 27 phonemically distinctive vowels , and its prosody is characterized by the distinctive phenomenon stød , a kind of laryngeal phonation type . Due to the many pronunciation differences that set Danish apart from its neighboring languages, particularly the vowels, difficult prosody and "weakly" pronounced consonants, it is sometimes considered to be
2964-597: A whole. Further, more precipitation in the northwest had been falling as rain instead of snow, with a fourfold increase in rain since 1980. Rain is warmer than snow and forms darker and less thermally insulating ice layer once it does freeze on the ice sheet. It is particularly damaging when it falls due to late-summer cyclones, whose increasing occurrence has been overlooked by the earlier models. There has also been an increase in water vapor , which paradoxically increases melting by making it easier for heat to radiate downwards through moist, as opposed to dry, air. Altogether,
3120-700: Is a West Germanic language descended from Old English. Old Norse exerted a strong influence on Old English in the early medieval period. The shared Germanic heritage of Danish and English is demonstrated with many common words that are very similar in the two languages. For example, when written, commonly used Danish verbs, nouns, and prepositions such as have , over , under , for , give , flag , salt , and arm are easily recognizable to English speakers. Similarly, some other words are almost identical to their Scots equivalents, e.g. kirke (Scots kirk , i.e., 'church') or barn (Scots and northern English bairn , i.e. 'child'). In addition,
3276-501: Is about 0.5-27 billion tonnes of pure carbon underneath the entire ice sheet, and much less within it. This is much less than the 1400–1650 billion tonnes contained within the Arctic permafrost , or the annual anthropogenic emissions of around 40 billion tonnes of CO 2 . ) Yet, the release of this carbon through meltwater can still act as a climate change feedback if it increases overall carbon dioxide emissions. There
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#17327831873523432-595: Is almost 2,900 kilometres (1,800 mi) long in a north–south direction, with a maximum width of 1,100 kilometres (680 mi) at a latitude of 77°N , near its northern edge. The ice sheet covers 1,710,000 square kilometres (660,000 sq mi), around 80% of the surface of Greenland , or about 12% of the area of the Antarctic ice sheet . The term 'Greenland ice sheet' is often shortened to GIS or GrIS in scientific literature . Greenland has had major glaciers and ice caps for at least 18 million years, but
3588-693: Is exposed. Uncertainty about the snow line is one of the factors making it hard to predict each melting season in advance. A notable example of ice accumulation rates above the snow line is provided by Glacier Girl , a Lockheed P-38 Lightning fighter plane which had crashed early in World War II and was recovered in 1992, by which point it had been buried under 268 ft ( 81 + 1 ⁄ 2 m) of ice. Another example occurred in 2017, when an Airbus A380 had to make an emergency landing in Canada after one of its jet engines exploded while it
3744-430: Is its closest relative. East Germanic languages West Germanic languages Icelandic Faroese Norwegian Danish Swedish Approximately 2,000 uncompounded Danish words are derived from Old Norse and ultimately from Proto Indo-European . Of these 2,000, 1,200 are nouns, 500 are verbs and 180 are adjectives. Danish has also absorbed many loanwords , most of which were borrowed from Low German of
3900-641: Is known as ice calving . Sediment released from calved and melting ice sinks accumulates on the seafloor, and sediment cores from places such as the Fram Strait provide long records of glaciation at Greenland. While there is evidence of large glaciers in Greenland for most of the past 18 million years, these ice bodies were probably similar to various smaller modern examples, such as Maniitsoq and Flade Isblink , which cover 76,000 and 100,000 square kilometres (29,000 and 39,000 sq mi) around
4056-403: Is known that when the weather became colder the three men took the same route along the coast of the farthest northeast point of Greenland where depots had been laid. By then they had only four dogs and a sled. They reached the cliffs of Mallemuk Mountain but found open water that made it impossible for them to travel straight southwards, so the exhausted men had to travel inland on 19 October 1907,
4212-458: Is one known area, at Russell Glacier , where meltwater carbon is released into the atmosphere in the form of methane (see arctic methane emissions ), which has a much larger global warming potential than carbon dioxide. However, the area also harbours large numbers of methanotrophic bacteria, which limit those methane emissions. In 2021, research claimed that there must be mineral deposits of mercury (a highly toxic heavy metal ) beneath
4368-610: Is subtle, it already causes East Coast of the United States to experience faster sea level rise than the global average. At the same time, Greenland itself would experience isostatic rebound as its ice sheet shrinks and its ground pressure becomes lighter. Similarly, a reduced mass of ice would exert a lower gravitational pull on the coastal waters relative to the other land masses. These two processes would cause sea level around Greenland's own coasts to fall, even as it rises elsewhere. The opposite of this phenomenon happened when
4524-585: Is underestimated unless the smaller glaciers are accounted for. By 2023, the rate of ice loss across Greenland's coasts had doubled in the two decades since 2000, in large part due to the accelerated losses from smaller glaciers. Since the early 2000s, glaciologists have concluded that glacier retreat in Greenland is accelerating too quickly to be explained by a linear increase in melting in response to greater surface temperatures alone, and that additional mechanisms must also be at work. Rapid calving events at
4680-648: Is very effective at reflecting sunlight. Ice-albedo feedback means that as the temperatures increase, this causes more ice to melt and either reveal bare ground or even just to form darker melt ponds, both of which act to reduce albedo, which accelerates the warming and contributes to further melting. This is taken into account by the climate models , which estimate that a total loss of the ice sheet would increase global temperature by 0.13 °C (0.23 °F), while Greenland's local temperatures would increase by between 0.5 °C (0.90 °F) and 3 °C (5.4 °F). Even incomplete melting already has some impact on
4836-436: The skarre-R , the uvular R sound ( [ʁ] ), began spreading through Denmark, likely through influence from Parisian French and German. It affected all of the areas where Danish had been influential, including all of Denmark, Southern Sweden, and coastal southern Norway. In the 18th century, Danish philology was advanced by Rasmus Rask , who pioneered the disciplines of comparative and historical linguistics, and wrote
Denmark expedition - Misplaced Pages Continue
4992-623: The Bible in Danish, the Bible of Christian II translated by Christiern Pedersen , was published in 1550. Pedersen's orthographic choices set the de facto standard for subsequent writing in Danish. From around 1500, several printing presses were in operation in Denmark publishing in Danish and other languages. In the period after 1550, presses in Copenhagen dominated the publication of material in
5148-497: The Faeroe Islands along with a hundred sled dogs . Among the scientists was German meteorologist Alfred Wegener . Georg Carl Amdrup was in charge of writing the official history of the expedition. In the autumn of 1906, northbound sled journeys began in order to lay depots along the route of the long northern explorations in the spring of the following year. Finally, ten sleds led by Mylius-Erichsen left Danmarkshavn at
5304-583: The Kaiser Franz Joseph Fjord . Time permitting, the expedition would also attempt a westward crossing of the inland ice. In addition, Robert Peary's claim that a channel running from east to west separated northernmost Greenland from the mainland further south – the (non-existent) so-called " Peary Channel " – was to be investigated. A committee of authorities on Greenland, including Gustav Frederik Holm , Carl Ryder , Georg Carl Amdrup and Thomas Vilhelm Garde , advised Mylius-Erichsen on
5460-570: The Late Middle Ages . Out of the 500 most frequently used Danish words, 100 are loans from Middle Low German; this is because Low German was the second official language of Denmark–Norway. In the 17th and 18th centuries, standard German and French superseded Low German influence, and in the 20th century, English became the main supplier of loanwords, especially after World War II . Although many old Nordic words remain, some were replaced with borrowed synonyms, for example æde (to eat)
5616-523: The Old Norse language ; Danish and Swedish are also classified as East Scandinavian or East Nordic languages. Scandinavian languages are often considered a dialect continuum , where no sharp dividing lines are seen between the different vernacular languages. Like Norwegian and Swedish, Danish was significantly influenced by Low German in the Middle Ages, and has been influenced by English since
5772-469: The Paris Agreement goals are largely fulfilled, SSP1-2.6, adds around 6 cm ( 2 + 1 ⁄ 2 in) and no more than 15 cm (6 in), with a small chance of the ice sheet gaining mass and thus reducing the sea levels by around 2 cm (1 in). Some scientists, led by James Hansen , have claimed that the ice sheets can disintegrate substantially faster than estimated by
5928-533: The Pliocene , formed a lower planation surface at 500 to 1000 meters above sea level. A third stage of uplift created multiple valleys and fjords below the planation surfaces. This uplift intensified glaciation due to increased orographic precipitation and cooler surface temperatures , allowing ice to accumulate and persist. As recently as 3 million years ago, during the Pliocene warm period, Greenland's ice
6084-688: The Viking Era . Danish, together with Swedish, derives from the East Norse dialect group , while the Middle Norwegian language (before the influence of Danish) and Norwegian Bokmål are classified as West Norse along with Faroese and Icelandic . A more recent classification based on mutual intelligibility separates modern spoken Danish, Norwegian , and Swedish as "mainland (or continental ) Scandinavian", while Icelandic and Faroese are classified as "insular Scandinavian". Although
6240-582: The West Antarctic Ice Sheet have been accelerating due to its vulnerable Thwaites and Pine Island Glaciers , and the Antarctic contribution to sea level rise is expected to overtake that of Greenland later this century. Retreat of outlet glaciers as they shed ice into the Arctic is a large factor in the decline of Greenland's ice sheet. Estimates suggest that losses from glaciers explain between 49% and 66.8% of observed ice loss since
6396-544: The Zealand dialect Introductio ad lingvam Danicam puta selandicam ; and in 1685 the first Danish grammar written in Danish, Den Danske Sprog-Kunst ("The Art of the Danish Language") by Peder Syv . Major authors from this period are Thomas Kingo , poet and psalmist, and Leonora Christina Ulfeldt , whose novel Jammersminde ( Remembered Woes ) is considered a literary masterpiece by scholars. Orthography
Denmark expedition - Misplaced Pages Continue
6552-435: The effects of climate change on the water cycle could increase snowfall over Greenland, and thus further delay this transition. This hypothesis was difficult to test in the 2000s due to the poor state of long-term precipitation records over the ice sheet. By 2019, it was found that while there was an increase in snowfall over southwest Greenland, there had been a substantial decrease in precipitation over western Greenland as
6708-467: The firn layer at night, which can increase total meltwater runoff by over 30%. Thin, water-rich clouds have the worst impact, and they were the most prominent in July 2012. Ice cores had shown that the last time a melting event of the same magnitude as in 2012 took place was in 1889, and some glaciologists had expressed hope that 2012 was part of a 150-year cycle. This was disproven in summer 2019, when
6864-469: The ice sheet models , but even their projections also have much of Greenland, whose total size amounts to 7.4 m (24 ft) of sea level rise, survive the 21st century. A 2016 paper from Hansen claimed that Greenland ice loss could add around 33 cm (13 in) by 2060, in addition to double that figure from the Antarctic ice sheet , if the CO 2 concentration exceeded 600 parts per million , which
7020-402: The introduction of the printing press , a standard language was developed which was based on the educated dialect of Copenhagen and Malmö . It spread through use in the education system and administration, though German and Latin continued to be the most important written languages well into the 17th century. Following the loss of territory to Germany and Sweden, a nationalist movement adopted
7176-439: The sea ice and icebergs immediately off-shore were able to survive for longer, and thus helped to stabilize the glacier. Likewise, the rapid retreat and then slowdown of Helheim and Kangerdlugssuaq has also been connected to the respective warming and cooling of nearby currents. At Petermann Glacier, the rapid rate of retreat has been linked to the topography of its grounding line, which appears to shift back and forth by around
7332-442: The water cycle at the time, while air bubbles frozen within the ice core provide a snapshot of the gas and particulate composition of the atmosphere through time. When properly analyzed, ice cores provide a wealth of proxies suitable for reconstructing the past temperature record , precipitation patterns, volcanic eruptions , solar variation , ocean primary production , and even changes in soil vegetation cover and
7488-479: The 1930s and 1940s than in the decades immediately before or after. More complete data sets have established trends of warming and ice loss starting from 1900 (well after the start of the Industrial Revolution and its impact on global carbon dioxide levels ) and a trend of strong warming starting around 1979, in line with concurrent observed Arctic sea ice decline . In 1995– 1999, central Greenland
7644-459: The 1980s. Net loss of ice was already observed across 70% of the ice sheet margins by the 1990s, with thinning detected as the glaciers started to lose height. Between 1998 and 2006, thinning occurred four times faster for coastal glaciers compared to the early 1990s, falling at rates between 1 m ( 3 + 1 ⁄ 2 ft) and 10 m (33 ft) per year, while the landlocked glaciers experienced almost no such acceleration. One of
7800-541: The 2000s, reaching ~187 Gt/yr in 2000–2010, and an average mass loss during 2010–2018 of 286 Gt per year. Half of the ice sheet's observed net loss (3,902 gigatons (Gt) of ice between 1992 and 2018, or approximately 0.13% of its total mass ) happened during those 8 years. When converted to sea level rise equivalent, the Greenland ice sheet contributed about 13.7 mm since 1972. Between 2012 and 2017, it contributed 0.68 mm per year, compared to 0.07 mm per year between 1992 and 1997. Greenland's net contribution for
7956-497: The 2012–2016 period was equivalent to 37% of sea level rise from land ice sources (excluding thermal expansion). These melt rates are comparable to the largest experienced by the ice sheet over the past 12,000 years. Currently, the Greenland ice sheet loses more mass every year than the Antarctic ice sheet , because of its position in the Arctic , where it is subject to intense regional amplification of warming . Ice losses from
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#17327831873528112-579: The 9th century with the younger futhark . Possibly as far back as the seventh century, the common Norse language began to undergo changes that did not spread to all of Scandinavia, resulting in the appearance of two dialect areas, Old West Norse ( Norway and Iceland ) and Old East Norse ( Denmark and Sweden ). Most of the changes separating East Norse from West Norse started as innovations in Denmark, that spread through Scania into Sweden and by maritime contact to southern Norway. A change that separated Old East Norse (Runic Swedish/Danish) from Old West Norse
8268-575: The AMOC ultimately stabilizes under RCP 4.5, but it continues to decline under RCP 8.5: the average decline by 2290–2300 is 74%, and there is 44% likelihood of an outright collapse in that scenario, with a wide range of adverse effects. In 2021, the IPCC Sixth Assessment Report estimated that under SSP5-8.5 , the scenario associated with the highest global warming, Greenland ice sheet melt would add around 13 cm (5 in) to
8424-400: The AMOC would weaken by around 18% (with a range of potential weakening between 3% and 34%) under Representative Concentration Pathway 4.5, which is most akin to the current trajectory, while it would weaken by 37% (with a range between 15% and 65%) under Representative Concentration Pathway 8.5, which assumes continually increasing emissions. If the two scenarios are extended past 2100, then
8580-468: The Arctic, including Greenland, to warm three to four times more than the global average: thus, while a period like the Eemian interglacial 130,000–115,000 years ago was not much warmer than today globally, the ice sheet was 8 °C (14 °F) warmer, and its northwest part was 130 ± 300 meters lower than it is at present. Some estimates suggest that the most vulnerable and fastest-receding parts of
8736-531: The Danish language, and also started a period of homogenization, whereby the Copenhagen standard language gradually displaced the regional vernacular languages. Throughout the 19th century, Danes emigrated, establishing small expatriate communities in the Americas, particularly in the United States, Canada, and Argentina, where memory and some use of Danish remains today. After the Schleswig referendum in 1920 ,
8892-517: The Danish language. Herrer og Narre have frit Sprog . "Lords and jesters have free speech." Peder Syv , proverbs Following the first Bible translation, the development of Danish as a written language , as a language of religion, administration, and public discourse accelerated. In the second half of the 17th century, grammarians elaborated grammars of Danish, first among them Rasmus Bartholin 's 1657 Latin grammar De studio lingvæ danicæ ; then Laurids Olufsen Kock 's 1660 grammar of
9048-407: The Danish tongue." Heimskringla by Snorri Sturluson By the eighth century, the common Germanic language of Scandinavia, Proto-Norse , had undergone some changes and evolved into Old Norse . This language was generally called the "Danish tongue" ( Dǫnsk tunga ), or "Norse language" ( Norrœnt mál ). Norse was written in the runic alphabet , first with the elder futhark and from
9204-493: The Denmark expedition was not a failure. It achieved its main cartographic objectives and succeeded in exploring the vast region, drawing accurate charts of formerly unexplored coastlines and fjords , naming numerous geographic features, and gathering a wealth of scientific data. The two-year expedition was conceived and led by Ludvig Mylius-Erichsen, who had previously led the 'Literary Expedition' to Northwest Greenland together with Knud Rasmussen in 1902–1904. The main target of
9360-406: The Denmark expedition was to map the last blank sections of the coastline of northeastern Greenland, between Cape Bridgman , near Robert Peary 's easternmost geographic exploration in the north, and Cape Bismarck , the northernmost point reached by Carl Koldewey in the east. Beginning in the 1700s Greenland had slowly been mapped section by section, but the harsh climate in the far northeast and
9516-647: The Faroe Islands , and the northern German region of Southern Schleswig , where it has minority language status. Minor Danish-speaking communities are also found in Norway , Sweden , the United States , Canada , Brazil , and Argentina . Along with the other North Germanic languages, Danish is a descendant of Old Norse , the common language of the Germanic peoples who lived in Scandinavia during
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#17327831873529672-450: The Nordic countries have the opportunity to use their native language when interacting with official bodies in other Nordic countries without being liable for any interpretation or translation costs. Greenland ice sheet The Greenland ice sheet is an ice sheet which forms the second largest body of ice in the world. It is an average of 1.67 km (1.0 mi) thick, and over 3 km (1.9 mi) thick at its maximum. It
9828-710: The Old Norse word for "island". This monophthongization started in Jutland and spread eastward, having spread throughout Denmark and most of Sweden by 1100. Through Danish conquest, Old East Norse was once widely spoken in the northeast counties of England . Many words derived from Norse, such as "gate" ( gade ) for street, still survive in Yorkshire , the East Midlands and East Anglia, and parts of eastern England colonized by Danish Vikings . The city of York
9984-484: The absence of existing large crevasses that are normally thought to be necessary for their formation. Currently, the total accumulation of ice on the surface of Greenland ice sheet is larger than either outlet glacier losses individually or surface melting during the summer, and it is the combination of both which causes net annual loss. For instance, the ice sheet's interior thickened by an average of 6 cm (2.4 in) each year between 1994 and 2005, in part due to
10140-600: The area, eventually outnumbering the Danish speakers. The political loss of territory sparked a period of intense nationalism in Denmark, coinciding with the so-called " Golden Age " of Danish culture. Authors such as N.F.S. Grundtvig emphasized the role of language in creating national belonging. Some of the most cherished Danish-language authors of this period are existential philosopher Søren Kierkegaard and prolific fairy tale author Hans Christian Andersen . The influence of popular literary role models, together with increased requirements of education did much to strengthen
10296-524: The associated wildfire frequency. The ice cores from Greenland also record human impact, such as lead production during the time of Ancient Greece and the Roman Empire . From the 1960s to the 1980s an area in the North Atlantic which included southern Greenland was one of the few locations in the world which showed cooling rather than warming. This location was relatively warmer in
10452-560: The authoritative work of the 1906–08 Denmark expedition. Danish language Nordic Council Danish ( / ˈ d eɪ n ɪ ʃ / , DAY -nish ; endonym : dansk pronounced [ˈtænˀsk] , dansk sprog [ˈtænˀsk ˈspʁɔwˀ] ) is a North Germanic language from the Indo-European language family spoken by about six million people, principally in and around Denmark . Communities of Danish speakers are also found in Greenland ,
10608-401: The base of the glaciers and generates higher basal pressure, which collectively reduces friction and accelerates glacial motion , including the rate of ice calving . This mechanism was observed at Sermeq Kujalleq in 1998 and 1999, where flow increased by up to 20% for two to three months. However, some research suggests that this mechanism only applies to certain small glaciers, rather than to
10764-586: The calving front. While the models generally consider the impact from meltwater run-off as secondary to ocean warming, observations of 13 glaciers found that meltwater plumes play a greater role for glaciers with shallow grounding lines. Further, 2022 research suggests that the warming from plumes had a greater impact on underwater melting across northwest Greenland. Finally, it has been shown that meltwater can also flow through cracks that are too small to be picked up by most research tools - only 2 cm (1 in) wide. Such cracks do not connect to bedrock through
10920-411: The central Greenland ice sheet, even the most extensive melting event can only affect a small fraction of it before the start of the freezing season, and so they are considered "short-term variability" in the scientific literature. Nevertheless, their existence is important: the fact that the current models underestimate the extent and frequency of such events is considered to be one of the main reasons why
11076-420: The coast up to Danmark Fjord in the far north. The Danmark left Greenland on 21 July, arriving in Copenhagen one month later. Since the unfortunate circumstances of Mylius-Erichsen's death cast a pall over the whole expedition, its results didn't receive the attention they deserved. Even so, over 51 reports were published by its members, including those by numerous scientists. A number of them continued to work in
11232-453: The coast, in the direction that they deemed would lead them to Gletscher Cape and Navy Cliff — at the head of Independence Fjord . Meanwhile the other team — with Johan Peter Koch , Aage Bertelsen and Tobias Gabrielsen — sped northwestwards across the sea ice towards Cape Bridgman in order to map the uncharted coast sections of eastern Peary Land . Mylius-Erichsen entered the unknown Danmark Fjord without having doubts about where it
11388-426: The current ice sheet volume was left during those geologically recent periods, when the temperatures were less than 2.5 °C (4.5 °F) warmer than preindustrial conditions. This contradicts how climate models typically simulate the continuous presence of solid ice under those conditions. Analysis of the ~100,000-year records obtained from 3 km (1.9 mi) long ice cores drilled between 1989 and 1993 into
11544-511: The day the sun disappeared below the horizon. Walking on the ice in the darkness Høeg Hagen was the first to die of exhaustion in the Nioghalvfjerd Fjord area, followed shortly thereafter by Mylius-Erichsen. Jørgen Brønlund reached Lambert Land in the moonlight and his body was found there by Koch in mid-March 1908. Brønlund had his diary and Hagen's cartographic sketches. He was buried at Kap Bergendahl in southeast Lambert Land,
11700-543: The difficult ice conditions off the shore had prevented the cartography of the vast zone. The expedition aimed to gather scientific information on the unexplored area during a period of two years, including information on any remaining Northeast-Greenland Inuit, last seen by Royal Navy Captain Douglas Clavering in 1823 further south down the coast in Clavering Island . The strategy of the expedition
11856-485: The dog sleds — led by Gustav Thostrup and Alfred Wegener — mapped the shoreline, while the other one — led by Henning Bistrup and Carl Johan Ring — mapped the numerous offshore islands. As the six northbound dog sleds sped along the eastern coast of the Crown Prince Christian Land peninsula, Mylius-Erichsen was feeling uneasy because the shore was leading them further to the northeast, which
12012-546: The end of March 1907, heading north on the coastal ice. Along Jokel Bay , where the Greenland ice sheet comes down to the sea, buckling and cracking the ice near the shore, travelling was difficult and sleds broke and had to be continually repaired. The harsh ice conditions continued along Hovgaard Island further north. At Mallemuk Mountain in SE Holm Land the coastal ice of the Dijmphna Sound gave way to
12168-437: The end of the century. If there are no reductions in emissions, melting would add around 13 cm (5 in) by 2100, with a worst-case of about 33 cm (13 in). For comparison, melting has so far contributed 1.4 cm ( 1 ⁄ 2 in) since 1972, while sea level rise from all sources was 15–25 cm (6–10 in) between 1901 and 2018. If all 2,900,000 cubic kilometres (696,000 cu mi) of
12324-508: The entire ice sheet but may still reach several hundred meters down from the surface. Their presence is important, as it weakens the ice sheet, conducts more heat directly through the ice, and allows it to flow faster. This recent research is not currently captured in models. One of the scientists behind these findings, Alun Hubbard, described finding moulins where "current scientific understanding doesn’t accommodate" their presence, because it disregards how they may develop from hairline cracks in
12480-508: The exclusive use of rigsdansk , the High Copenhagen Standard, in national broadcasting, the traditional dialects came under increased pressure. In the 20th century, they have all but disappeared, and the standard language has extended throughout the country. Minor regional pronunciation variation of the standard language, sometimes called regionssprog ("regional languages") remain, and are in some cases vital. Today,
12636-451: The first English-language grammar of Danish. Literary Danish continued to develop with the works of Ludvig Holberg , whose plays and historical and scientific works laid the foundation for the Danish literary canon. With the Danish colonization of Greenland by Hans Egede , Danish became the administrative and religious language there, while Iceland and the Faroe Islands had the status of Danish colonies with Danish as an official language until
12792-504: The first team of researchers as a reagent . However, there is still a risk of toxic waste being released from Camp Century , formerly a United States military site built to carry nuclear weapons for the Project Iceworm . The project was cancelled, but the site was never cleaned up, and it now threatens to pollute the meltwater with nuclear waste , 20,000 liters of chemical waste and 24 million liters of untreated sewage as
12948-507: The glacier disintegrated, and the glacier shed 94 square kilometres (36 sq mi) of ice between 2001 and 2005. The ice flow reached 45 metres (148 ft) per day in 2012, but slowed down substantially afterwards, and showed mass gain between 2016 and 2019. Northern Greenland's Petermann Glacier is smaller in absolute terms, but experienced some of the most rapid degradation in recent decades. It lost 85 square kilometres (33 sq mi) of floating ice in 2000–2001, followed by
13104-459: The glacier's ice shelf had lost around 40% of its pre-2010 state, and it is considered unlikely to recover from further ice loss. In the early 2010s, some estimates suggested that tracking the largest glaciers would be sufficient to account for most of the ice loss. However, glacier dynamics can be hard to predict, as shown by the ice sheet's second largest glacier, Helheim Glacier . Its ice loss culminated in rapid retreat in 2005, associated with
13260-444: The global sea levels (with a likely (17%–83%) range of 9–18 cm ( 3 + 1 ⁄ 2 –7 in) and a very likely range ( 5–95% confidence level ) of 5–23 cm (2–9 in)), while the "moderate" SSP2-4.5 scenario adds 8 cm (3 in) with a likely and very likely range of 4–13 cm ( 1 + 1 ⁄ 2 –5 in) and 1–18 cm ( 1 ⁄ 2 –7 in), respectively. The optimistic scenario which assumes that
13416-414: The historical record, which spans from late 19th century to present. Some research suggests that Greenland's meltwater mainly benefits marine productivity not by adding carbon and iron, but through stirring up lower water layers that are rich in nitrates and thus bringing more of those nutrients to phytoplankton on the surface. As the outlet glaciers retreat inland, the meltwater will be less able to impact
13572-426: The history of Danish into a period from 800 AD to 1525 to be "Old Danish", which he subdivided into "Runic Danish" (800–1100), Early Middle Danish (1100–1350) and Late Middle Danish (1350–1525). Móðir Dyggva var Drótt, dóttir Danps konungs, sonar Rígs er fyrstr var konungr kallaðr á danska tungu . " Dyggvi 's mother was Drott, the daughter of king Danp, Ríg 's son, who was the first to be called king in
13728-425: The ice sheet (compared to 4% for Kangerlussuaq ), at speeds of ~20 metres (66 ft) per day. While it lost enough ice to retreat around 30 km (19 mi) between 1850 and 1964, its mass gain increased sufficiently to keep it in balance for the next 35 years, only to switch to rapid mass loss after 1997. By 2003, the average annual ice flow speed had almost doubled since 1997, as the ice tongue in front of
13884-486: The ice sheet formed in Greenland, its size remained similar to its current state. However, there have been 11 periods in Greenland's history when the ice sheet extended up to 120 km (75 mi) beyond its current boundaries; with the last one around 1 million years ago. The weight of the ice causes it to slowly "flow", unless it is stopped by a sufficiently large obstacle, such as a mountain . Greenland has many mountains near its coastline , which normally prevent
14040-493: The ice sheet from flowing further into the Arctic Ocean . The 11 previous episodes of glaciation are notable because the ice sheet grew large enough to flow over those mountains. Nowadays, the northwest and southeast margins of the ice sheet are the main areas where there are sufficient gaps in the mountains to enable the ice sheet to flow out to the ocean through outlet glaciers . These glaciers regularly shed ice in what
14196-623: The ice sheet gained mass during the Little Ice Age : increased weight attracted more water and flooded certain Viking settlements, likely playing a large role in the Viking abandonment soon afterwards. Notably, the ice sheet's massive size simultaneously makes it insensitive to temperature changes in the short run, yet also commits it to enormous changes down the line, as demonstrated by paleoclimate evidence. Polar amplification causes
14352-454: The ice sheet have already passed "a point of no return" around 1997, and will be committed to disappearance even if the temperature stops rising. A 2022 paper found that the 2000–2019 climate would already result in the loss of ~3.3% volume of the entire ice sheet in the future, committing it to an eventual 27 cm ( 10 + 1 ⁄ 2 in) of SLR, independent of any future temperature change. They have additionally estimated that if
14508-532: The ice sheet lost approximately 0.1% of its total mass (2900 Gt) during that year's melting season, with the net loss (464 Gt) setting another record. It became the first directly observed example of a "massive melting event", when the melting took place across practically the entire ice sheet surface, rather than specific areas. That event led to the counterintuitive discovery that cloud cover, which normally results in cooler temperature due to their albedo , actually interferes with meltwater refreezing in
14664-480: The ice sheet were to melt, it would increase global sea levels by ~7.4 m (24 ft). Global warming between 1.7 °C (3.1 °F) and 2.3 °C (4.1 °F) would likely make this melting inevitable. However, 1.5 °C (2.7 °F) would still cause ice loss equivalent to 1.4 m ( 4 + 1 ⁄ 2 ft) of sea level rise, and more ice will be lost if the temperatures exceed that level before declining. If global temperatures continue to rise,
14820-452: The ice sheet will likely disappear within 10,000 years. At very high warming, its future lifetime goes down to around 1,000 years. Ice sheets form through a process of glaciation , when the local climate is sufficiently cold that snow is able to accumulate from year to year. As the annual snow layers pile up, their weight gradually compresses the deeper levels of snow to firn and then to solid glacier ice over hundreds of years. Once
14976-451: The ice-albedo feedback. Besides the formation of darker melt ponds, warmer temperatures enable increasing growth of algae on the ice sheet's surface. Mats of algae are darker in colour than the surface of the ice, so they absorb more thermal radiation and increase the rate of ice melt. In 2018, it was found that the regions covered in dust , soot , and living microbes and algae altogether grew by 12% between 2000 and 2012. In 2020, it
15132-424: The language as a token of Danish identity, and the language experienced a strong surge in use and popularity, with major works of literature produced in the 18th and 19th centuries. Today, traditional Danish dialects have all but disappeared, though regional variants of the standard language exist. The main differences in language are between generations, with youth language being particularly innovative. Danish has
15288-547: The language of the courts. Since 1997, public authorities have been obliged to follow the official spelling system laid out in the Orthography Law. In the 21st century, discussions have been held with a view to create a law that would make Danish the official language of Denmark. In addition, a noticeable community of Danish speakers is in Southern Schleswig , the portion of Germany bordering Denmark, and
15444-431: The largest glaciers match what was first described as the "Jakobshavn effect" in 1986: thinning causes the glacier to be more buoyant, reducing friction that would otherwise impede its retreat, and resulting in a force imbalance at the calving front, with an increase in velocity spread across the mass of the glacier. The overall acceleration of Jakobshavn Isbrae and other glaciers from 1997 onwards had been attributed to
15600-421: The largest outlet glaciers, and may have only a marginal impact on ice loss trends. Secondly, once meltwater flows into the ocean, it can still impact the glaciers by interacting with ocean water and altering its local circulation - even in the absence of any ocean warming. In certain fjords , large meltwater flows from beneath the ice may mix with ocean water to create turbulent plumes that can be damaging to
15756-495: The last year the Greenland ice sheet saw net mass gain. As of 2022, the Greenland ice sheet had been losing ice for 26 years in a row, and temperatures there had been the highest in the entire past last millennium – about 1.5 °C (2.7 °F) warmer than the 20th century average. Several factors determine the net rate of ice sheet growth or decline. These are: When the IPCC Third Assessment Report
15912-509: The leader of the expedition again — he and his team arrived at the ship almost one month later. Mylius-Erichsen travelled west following the southern side of Independence Fjord and reached Academy Glacier at the head of Independence Fjord on 1 June, discovering that the Peary Channel did not exist. On the way back, the team explored Brønlund Fjord and Hagen Fjord . Sudden mild weather then impeded their progress, and when they reached
16068-536: The local fjords , and further out in the Labrador Sea , where 40% of the total primary production had been attributed to nutrients from meltwater. Since the 1950s, the acceleration of Greenland melt caused by climate change has already been increasing productivity in waters off the North Icelandic Shelf, while productivity in Greenland's fjords is also higher than it had been at any point in
16224-502: The long unexplored fjord. Koch and Mylius-Erichsen considered the situation. It was getting late in the season and it would be dangerous to get stuck in the inhospitable area during the summer without adequate equipment and supplies. Melting ice would make travel back to Danmarkshavn impossible. Initially, Mylius-Erichsen agreed to go back with Koch to the ship, but then he took the fateful decision to head west, leaving on 28 May. Thus Koch departed without suspecting that he would never see
16380-409: The lower layers, which implies that benefit from the meltwater will diminish even as its volume grows. The impact of meltwater from Greenland goes beyond nutrient transport. For instance, meltwater also contains dissolved organic carbon , which comes from the microbial activity on the ice sheet's surface, and, to a lesser extent, from the remnants of ancient soil and vegetation beneath the ice. There
16536-407: The major varieties of Standard Danish are High Copenhagen Standard, associated with elderly, well to-do, and well educated people of the capital, and low Copenhagen speech traditionally associated with the working class, but today adopted as the prestige variety of the younger generations. Also, in the 21st century, the influence of immigration has had linguistic consequences, such as the emergence of
16692-416: The melt extent staying at 337,000 sq mi (872,826.0 km ). At that time, rain fell for 13 hours at Greenland's Summit Station, located at 10,551 ft (3,215.9 m) elevation. Researchers had no rain gauges to measure the rainfall, because temperatures at the summit have risen above freezing only three times since 1989 and it had never rained there before. Due to the enormous thickness of
16848-580: The melt progresses. Finally, increased quantities of fresh meltwater can affect ocean circulation . Some scientists have connected this increased discharge from Greenland with the so-called cold blob in the North Atlantic , which is in turn connected to Atlantic meridional overturning circulation , or AMOC, and its apparent slowdown. In 2016, a study attempted to improve forecasts of future AMOC changes by incorporating better simulation of Greenland trends into projections from eight state-of-the-art climate models . That research found that by 2090–2100,
17004-426: The melt zone below the snow line, where summer warmth turns snow and ice into slush and melt ponds , has been expanding at an accelerating rate since the beginning of detailed measurements in 1979. By 2002, its area was found to have increased by 16% since 1979, and the annual melting season broke all previous records. Another record was set in July 2012, when the melt zone extended to 97% of the ice sheet's cover, and
17160-422: The mid-20th century. Moders navn er vort Hjertesprog, kun løs er al fremmed Tale. Det alene i mund og bog, kan vække et folk af dvale. "Mother's name is our hearts' tongue, only idle is all foreign speech It alone, in mouth or in book, can rouse a people from sleep." N.F.S. Grundtvig , "Modersmaalet" Following the loss of Schleswig to Germany, a sharp influx of German speakers moved into
17316-539: The most dramatic examples of thinning was in the southeast, at Kangerlussuaq Glacier . It is over 20 mi (32 km) long, 4.5 mi (7 km) wide and around 1 km ( 1 ⁄ 2 mi) thick, which makes it the third largest glacier in Greenland. Between 1993 and 1998, parts of the glacier within 5 km (3 mi) of the coast lost 50 m (164 ft) in height. Its observed ice flow speed went from 3.1–3.7 mi (5–6 km) per year in 1988–1995 to 8.7 mi (14 km) per year in 2005, which
17472-535: The observed ice sheet decline in Greenland and Antarctica tracks the worst-case rather than the moderate scenarios of the IPCC Fifth Assessment Report 's sea-level rise projections . Some of the most recent scientific projections of Greenland melt now include an extreme scenario where a massive melting event occurs every year across the studied period (i.e. every year between now and 2100 or between now and 2300), to illustrate that such
17628-474: The original plan to move the ship to Kaiser Franz Joseph Fjord in the second year was called off, Trolle carried on with the objectives of the expedition in the area during the remaining time. An exploration team was sent in April 1908 to Ardencaple Fjord , where the inner reaches had not yet been explored because previous expeditions could not go beyond its mouth on account of deep snow. A second weather station
17784-407: The other hand, the three largest glaciers - Jakobshavn, Helheim, and Kangerlussuaq - are all located in the southern half of the ice sheet, and just the three of them are expected to add 9.1–14.9 mm under RCP 8.5. Similarly, 2013 estimates suggested that by 2200, they and another large glacier would add 29 to 49 millimetres by 2200 under RCP 8.5, or 19 to 30 millimetres under RCP 4.5. Altogether,
17940-442: The periphery. Conditions in Greenland were not initially suitable for a single coherent ice sheet to develop, but this began to change around 10 million years ago , during the middle Miocene , when the two passive continental margins which now form the uplands of West and East Greenland experienced uplift , and ultimately formed the upper planation surface at a height of 2000 to 3000 meter above sea level . Later uplift, during
18096-666: The preparation of the expedition. The expedition travelled to Greenland aboard the Danmark , reaching a sheltered place in southern Germania Land in August 1906 and establishing its main base there, Danmarkshavn , which was named after the ship. The captain of the ship was Lieutenant Alf Trolle of the Danish Navy and the doctor Johannes Lindhard. Expedition members included a very large staff of mostly Danish scientists, as well as West Greenlanders who came aboard in Iceland and
18252-613: The same field, returning to Greenland in the decades that followed, such as Peter Freuchen in the Thule Expeditions , as well as J.P. Koch, who led the 1912–13 Danish Expedition to Queen Louise Land with A. Wegener. In 1929 Wegener would return to Greenland for the German Greenland Expedition . The Danske Islands were given their name by John Haller during the 1956–1958 Expedition to East Greenland led by Lauge Koch , in order to pay due homage to
18408-478: The seas annually, which was substantially larger than the liquid meltwater input from the Antarctic ice sheet , and equivalent to 0.7% of freshwater entering the oceans from all of the world's rivers . This meltwater is not pure, and contains a range of elements - most notably iron , about half of which (around 0.3 million tons every year) is bioavailable as a nutrient for phytoplankton . Thus, meltwater from Greenland enhances ocean primary production , both in
18564-472: The shared written standard language remained). With the introduction of absolutism in 1660, the Danish state was further integrated, and the language of the Danish chancellery, a Zealandic variety with German and French influence, became the de facto official standard language , especially in writing—this was the original so-called rigsdansk ("Danish of the Realm"). Also, beginning in the mid-18th century,
18720-529: The single largest contribution to 21st century ice loss in Greenland is expected to be from the northwest and central west streams (the latter including Jakobshavn), and glacier retreat will be responsible for at least half of the total ice loss, as opposed to earlier studies which suggested that surface melting would become dominant later this century. If Greenland were to lose all of its coastal glaciers, though, then whether or not it will continue to shrink will be entirely determined by whether its surface melting in
18876-408: The smaller glaciers were losing more ice to such melting than normal calving processes, leading to rapid retreat. Conversely, Jakobshavn Isbrae is sensitive to changes in ocean temperature as it experiences elevated exposure through a deep subglacial trench. This sensitivity meant that an influx of cooler ocean water to its location was responsible for its slowdown after 2015, in large part because
19032-443: The southwestern ice sheet, because of the exceptional concentrations in meltwater entering the local fjords . If confirmed, these concentrations would have equalled up to 10% of mercury in all of the world's rivers. In 2024, a follow-up study found only "very low" concentrations in meltwater from 21 locations. It concluded that the 2021 findings were best explained by accidental sample contamination with mercury(II) chloride , used by
19188-472: The spot where he was found, which is today known as Brønlund's Grave ( Danish : Brønlunds Grav ). Brønlund was only some 140 miles as the crow flies from Germania land. The expedition had covered 350 miles of the 500 that they needed to cover from Navy Cliff to Germania Land. When the death of expedition leader Mylius-Erichsen was confirmed, Captain Alf Trolle took formal command of the venture. Although
19344-466: The summer consistently outweighs ice accumulation during winter. Under the highest-emission scenario, this could happen around 2055, well before the coastal glaciers are lost. Sea level rise from Greenland does not affect every coast equally. The south of the ice sheet is much more vulnerable than the other parts, and the quantities of ice involved mean that there is an impact on the deformation of Earth's crust and on Earth's rotation . While this effect
19500-569: The summit has revealed ice that is around ~1,000,000 years old. Sediment samples from the Labrador Sea provide evidence that nearly all of the south Greenland ice had melted around 400,000 years ago, during Marine Isotope Stage 11 . Other ice core samples from Camp Century in northwestern Greenland, show that the ice there melted at least once during the past 1.4 million years, during the Pleistocene , and did not return for at least 280,000 years. These findings suggest that less than 10% of
19656-515: The summit of Greenland's ice sheet, had provided evidence for geologically rapid changes in climate, and informed research on tipping points such as in the Atlantic meridional overturning circulation (AMOC). Ice cores provide valuable information about the past states of the ice sheet, and other kinds of paleoclimate data. Subtle differences in the oxygen isotope composition of the water molecules in ice cores can reveal important information about
19812-467: The surface melt and ice cliffs calve into the sea. Normally the ice sheet would be replenished by winter snowfall, but due to global warming the ice sheet is melting two to five times faster than before 1850, and snowfall has not kept up since 1996. If the Paris Agreement goal of staying below 2 °C (3.6 °F) is achieved, melting of Greenland ice alone would still add around 6 cm ( 2 + 1 ⁄ 2 in) to global sea level rise by
19968-491: The then-record melting seen on the ice sheet in 2012 were to become its new normal, then the ice sheet would be committed to around 78 cm ( 30 + 1 ⁄ 2 in) SLR. Another paper suggested that paleoclimate evidence from 400,000 years ago is consistent with ice losses from Greenland equivalent to at least 1.4 m ( 4 + 1 ⁄ 2 ft) of sea level rise in a climate with temperatures close to 1.5 °C (2.7 °F), which are now inevitable at least in
20124-486: The three languages can often understand the others fairly well, though studies have shown that the mutual intelligibility is asymmetric: Norwegian speakers generally understand both Danish and Swedish far better than Swedes or Danes understand each other. Concomitantly, Swedes and Danes understand Norwegian better than they understand each other's languages. Norwegian occupies the middle position in terms of intelligibility because of its shared border with Sweden, resulting in
20280-445: The turn of the 20th century. Danish itself can be divided into three main dialect areas: Jutlandic (West Danish), Insular Danish (including the standard variety), and East Danish (including Bornholmian and Scanian ). According to the view that Scandinavian is a dialect continuum, East Danish can be considered intermediary between Danish and Swedish, while Scanian can be considered a Swedified East Danish dialect, and Bornholmian
20436-411: The vernacular language to be accessible also to those who were not Latinate. The Jutlandic Law and Scanian Law were written in vernacular Danish in the early 13th century. Beginning in 1350, Danish began to be used as a language of administration, and new types of literature began to be written in the language, such as royal letters and testaments. The orthography in this period was not standardized nor
20592-469: The vernacular, such as the plural form of verbs, should be conserved in writing (i.e. han er "he is" vs. de ere "they are"). The East Danish provinces were lost to Sweden after the Second Treaty of Brömsebro (1645) after which they were gradually Swedified; just as Norway was politically severed from Denmark, beginning also a gradual end of Danish influence on Norwegian (influence through
20748-491: The warming of North Atlantic waters which melt the glacier fronts from underneath. While this warming had been going on since the 1950s, 1997 also saw a shift in circulation which brought relatively warmer currents from the Irminger Sea into closer contact with the glaciers of West Greenland. By 2016, waters across much of West Greenland's coastline had warmed by 1.6 °C (2.9 °F) relative to 1990s, and some of
20904-486: The weight of ice above it, may cause erosion , eventually leaving nothing but bedrock below the ice sheet. However, there are parts of the Greenland ice sheet, near the summit, where the ice sheet slides over a basal layer of ice which had frozen solid to the ground, preserving ancient soil , which can then be recovered by drilling. The oldest such soil was continuously covered by ice for around 2.7 million years, while another, 3 kilometres (1.9 mi) deep ice core from
21060-427: The western side of Danmark Fjord on 12 June, they found their way across the ice blocked by open water. They had relied on hunting for their sustenance in order to supplement their fast-dwindling provisions, but hunting was poor. The stony ground had worn their footwear and Brønlund summed up their desperate situation: "No food, no foot gear, and several hundred miles to the ship. Our prospects are very bad indeed." It
21216-516: The whore-bed with another man's wife and he comes away alive..." Jutlandic Law, 1241 In the medieval period, Danish emerged as a separate language from Swedish. The main written language was Latin, and the few Danish-language texts preserved from this period are written in the Latin alphabet, although the runic alphabet seems to have lingered in popular usage in some areas. The main text types written in this period are laws, which were formulated in
21372-440: The word by , meaning ‘village’ or ‘town’, occurs in many English place-names, such as Whitby and Selby , as remnants of the Viking occupation . During that period English adopted ‘are’, the third person plural form of the verb ‘to be’, as well as the personal pronouns ‘they’, ‘them’ and ‘their’ from contemporary Old Norse. Danish is largely mutually intelligible with Norwegian and Swedish . A proficient speaker of any of
21528-489: The written languages are compatible, spoken Danish is distinctly different from Norwegian and Swedish and thus the degree of mutual intelligibility with either is variable between regions and speakers . Until the 16th century, Danish was a continuum of dialects spoken from Southern Jutland and Schleswig to Scania with no standard variety or spelling conventions. With the Protestant Reformation and
21684-437: Was a territory ruled by Denmark–Norway , one of whose official languages was Danish. Though Danish ceased to be an official language in Iceland in 1944, it is still widely used and is a mandatory subject in school, taught as a second foreign language after English. No law stipulates an official language for Denmark, making Danish the de facto official language only. The Code of Civil Procedure does, however, lay down Danish as
21840-431: Was above Greenland; the engine's massive air intake fan was recovered from the ice sheet two years later, when it was already buried beneath 4 ft (1 m)of ice and snow. While summer surface melting has been increasing, it is still expected that it will be decades before melting will consistently exceed snow accumulation on its own. It is also hypothesized that the increase in global precipitation associated with
21996-469: Was already 2 °C (3.6 °F) warmer than it was in the 1950s. Between 1991 and 2004, average winter temperature at one location, Swiss Camp, rose almost 6 °C (11 °F). Consistent with this warming, the 1970s were the last decade when the Greenland ice sheet grew, gaining about 47 gigatonnes per year. From 1980–1990 there was an average annual mass loss of ~51 Gt/y. The period 1990–2000 showed an average annual loss of 41 Gt/y, with 1996 being
22152-400: Was also one of two official languages of Greenland (alongside Greenlandic ). Danish now acts as a lingua franca in Greenland, with a large percentage of native Greenlanders able to speak Danish as a second language (it was introduced into the education system as a compulsory language in 1928). About 10% of the population speaks Danish as their first language , due to immigration. Iceland
22308-482: Was demonstrated that the presence of algae, which is not accounted for by ice sheet models unlike soot and dust, had already been increasing annual melting by 10–13%. Additionally, as the ice sheet slowly gets lower due to melting, surface temperatures begin to increase and it becomes harder for snow to accumulate and turn to ice, in what is known as surface-elevation feedback. Even in 1993, Greenland's melt resulted in 300 cubic kilometers of fresh meltwater entering
22464-477: Was established at Mørkefjord , west of Danmarkshavn, in order to compare meteorological observations. Also, the islands, the glaciers, and the coastline of Dove Bay were explored, as well as mountains and lakes in Germania Land. Although no living Inuit were found, the expedition discovered abundant evidence of their former habitations, such as tent rings, winter dwellings, meat caches, and tools, all along
22620-416: Was heading. The team travelled southwestwards until the head of the fjord and, becoming aware that it was a dead end, they backtracked to the northeast. By the end of May Mylius-Erichsen's team was back again at the mouth of the fjord. As they met Koch's team at Cape Rigsdagen , already on their way back from Cape Bridgman , Mylius-Erichsen realized that they had wasted precious time and provisions by entering
22776-544: Was immediately controversial amongst the scientific community, while 2019 research from different scientists claimed a maximum of 33 cm (13 in) by 2100 under the worst-case climate change scenario. As with the present losses, not all parts of the ice sheet would contribute to them equally. For instance, it is estimated that on its own, the Northeast Greenland ice stream would contribute 1.3–1.5 cm by 2100 under RCP 4.5 and RCP 8.5, respectively. On
22932-473: Was limited to the highest peaks in the east and the south. Ice cover gradually expanded since then, until the atmospheric CO2 levels dropped to between 280 and 320 ppm 2.7–2.6 million years ago, by which time temperatures had dropped sufficiently for the disparate ice caps to connect and cover most of the island. The base of the ice sheet may be warm enough due to geothermal activity to have liquid water beneath it. This liquid water, under pressure from
23088-488: Was mostly supplanted by the Low German spise . As well as loanwords, new words can be freely formed by compounding existing words. In standard texts of contemporary Danish, Middle Low German loans account for about 16–17% of the vocabulary, Graeco-Latin loans 4–8%, French 2–4% and English about 1%. Danish and English are both Germanic languages. Danish is a North Germanic language descended from Old Norse, and English
23244-580: Was not what he had expected. The distance to their goal was increasing, while time and provisions were running out. Finally, at the end of April, they rounded the northeastern end of Greenland , an inconspicuous point where the ice slope of the Flade Isblink met the frozen sea, and began traveling northwestwards, in the direction they had hoped for. Shortly thereafter, they split into two teams of three dog sleds each; Ludvig Mylius-Erichsen, Niels Peter Høeg Hagen and Jørgen Brønlund, went westward hugging
23400-574: Was once the Viking settlement of Jorvik. Several other English words derive from Old East Norse, for example "knife" ( kniv ), "husband" ( husbond ), and "egg" ( æg ). The suffix "-by" for 'town' is common in place names in Yorkshire and the east Midlands, for example Selby, Whitby, Derby, and Grimsby. The word "dale" meaning valley is common in Yorkshire and Derbyshire placenames. Fangær man saar i hor seng mæth annæns mansz kunæ. oc kumær han burt liuænd... . "If one catches someone in
23556-415: Was published in 2001, the analysis of observations to date had shown that the ice accumulation of 520 ± 26 gigatonnes per year was offset by runoff and bottom melting equivalent to ice losses of 297±32 Gt/yr and 32±3 Gt/yr, and iceberg production of 235±33 Gt/yr, with a net loss of −44 ± 53 gigatonnes per year. Annual ice losses from the Greenland ice sheet accelerated in
23712-463: Was still not standardized and the principles for doing so were vigorously discussed among Danish philologists. The grammar of Jens Pedersen Høysgaard was the first to give a detailed analysis of Danish phonology and prosody, including a description of the stød . In this period, scholars were also discussing whether it was best to "write as one speaks" or to "speak as one writes", including whether archaic grammatical forms that had fallen out of use in
23868-469: Was the change of the diphthong æi (Old West Norse ei ) to the monophthong e , as in stæin to sten . This is reflected in runic inscriptions where the older read stain and the later stin . Also, a change of au as in dauðr into ø as in døðr occurred. This change is shown in runic inscriptions as a change from tauþr into tuþr . Moreover, the øy (Old West Norse ey ) diphthong changed into ø , as well, as in
24024-474: Was the spoken language, and the regional laws demonstrate the dialectal differences between the regions in which they were written. Throughout this period, Danish was in contact with Low German , and many Low German loan words were introduced in this period. With the Protestant Reformation in 1536, Danish also became the language of religion, which sparked a new interest in using Danish as
24180-484: Was then the fastest known flow of any glacier. The retreat of Kangerlussuaq slowed down by 2008, and showed some recovery until 2016–2018, when more rapid ice loss occurred. Greenland's other major outlet glaciers have also experienced rapid change in recent decades. Its single largest outlet glacier is Jakobshavn Isbræ ( Greenlandic : Sermeq Kujalleq ) in west Greenland, which has been observed by glaciologists for many decades. It historically sheds ice from 6.5% of
24336-410: Was to cross the sea ice barrier on the east coast of Greenland, sail with a ship as far north as possible, find a safe anchorage, establish a base with a meteorological station , and then go further north on dogsleds along the coastal ice. After the last unmapped coast of Greenland had been explored, which Mylius-Erichsen deemed could be done in a year, the expedition would move south to further explore
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