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Inje County

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Inje County ( Korean :  인제군 ; MR :  Inje-gun ) is a county in Gangwon Province, South Korea . It has the lowest population density of any South Korean county. The county seat is Inje-eup , which located near the center of the county.

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45-735: Inje is located in the north of Gangwon Province . Inje County has been called multiple names throughout its history. It was first known as Jeojokhyeon in the Goguryeo Kingdom , then Heejaehyeon in the Silla Kingdom , and Inje in the Goryeo Dynasty . The area was then known as Youngsohyeon and once again later on became Inje in the Joseon Dynasty . It was finally raised to the status of Inje county in August of 1896. At

90-685: A Csa climate well inland to ensure hot summers and cold winters. They are generally found in the highly elevated areas of south-eastern Turkey ( Hakkâri ), north-western Iran, northern Iraq, parts of Central Asia , parts of the High Atlas mountain range in central Morocco and very small parts of the Intermountain West in the United States. This climate zone does not exist at all in the Southern Hemisphere, where

135-614: A classification). More extreme and inland humid continental climates, sometimes known as "hyper-continental" climates, are found in northeast China , southern Siberia , Mongolia , Kazakhstan , most of the southern interior of Canada , and the Upper Midwest , where temperatures in the winter resemble those of adjacent subarctic climates (with long, drier, generally very cold winters) but have longer and generally warmer summers (in occasional cases, hot summers). A more moderate variety, found in places like Honshu , east-central China,

180-516: A marked reduction in wintry precipitation, which increases the chances of a wintertime drought ( w ). Snowfall occurs in all areas with a humid continental climate and in many such places is more common than rain during the height of winter. In places with sufficient wintertime precipitation, the snow cover is often deep. Most summer rainfall occurs during thunderstorms , and in North America and Asia an occasional tropical cyclone (or

225-739: A subarctic climate. In the Southern Hemisphere , it exists in well-defined areas only in the Southern Alps of New Zealand , in the Snowy Mountains of Australia in Kiandra, New South Wales and the Andes Mountains of Argentina and Chile . Since climate regimes tend to be dominated by vegetation of one region with relatively homogenous ecology, those that project climate change remap their results in

270-526: A thermal profile, but because of semi-arid precipitation portions of it are grouped into the BSk category. In Europe , it is found in much of Central Europe : Germany (in the east and southeast part of the country), Austria (generally below 700 m (2,297 ft)), Poland , Czech Republic , Slovakia , Hungary (generally above 100 m (328 ft)), Croatia (mostly Slavonia region), in much of Eastern Europe : Ukraine (the whole country except

315-424: Is 1,210 mm. Located on the border of Mt. [9] And on January 8, 2021, -29.1 °C was unofficially recorded at Hyangrobong, making it the coldest in the country. Instead, you might think summer is cool, but it's not at all. It would be better than the rear area, but even in summer, as long as it doesn't rain, 30 °C is so hot that it's standard. As mentioned above, during the heatwave in 2018, 37.7 °C

360-447: Is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers, and cold (sometimes severely cold in the northern areas) and snowy winters. Precipitation is usually distributed throughout the year, but often these regions do have dry seasons. The definition of this climate in terms of temperature

405-523: Is also sad that it took 102 steps (which has now been disbanded) to go to Gangwon Province at all, but it is natural that it is a very difficult area to serve. The dwelling is formed on a narrow flatland along the river, and the Inbukcheon River, which runs through Naerincheon Stream, Seohwa, and Wontong area, meets in Inje-eup and flows into Soyangho Lake. Inje-gun was Chuncheon because it

450-442: Is as follows: the mean temperature of the coldest month must be below 0 °C (32.0 °F) or −3 °C (26.6 °F) depending on the isotherm, and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). In addition, the location in question must not be semi-arid or arid . The cooler Dfb , Dwb , and Dsb subtypes are also known as hemiboreal climates. Although amount of snowfall

495-521: Is found in northern Kazakhstan , southern Siberia , parts of Mongolia , northern China , and highland elevations in the Koreas . Like its hot-summer counterpart, these climates are typically dry in the winter and bitterly cold due to the Siberian High (often with winter temperatures comparable to their nearby subarctic climates ), while summers are warm and long enough to avoid classification as

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540-467: Is less extreme than the most inland hyper-continental variety. Using the Köppen climate classification , a climate is classified as humid continental when the temperature of the coldest month is below 0 °C [32.0 °F] or −3 °C [26.6 °F] and there must be at least four months whose mean temperatures are at or above 10 °C (50 °F). These temperatures were not arbitrary. In Europe,

585-565: Is less seasonally uniform in the west. The western states of the western United States (namely Montana , Wyoming , parts of southern Idaho , most of Lincoln County in Eastern Washington , parts of Colorado , parts of Utah , isolated parts of northern New Mexico , western Nebraska , and parts of western North and South Dakota ) have thermal regimes which fit the Dfa climate type, but are quite dry, and are generally grouped with

630-640: Is located in the Taebaek Mountains and has a landscape dominated by flora. Many species inhabit several areas of the county, not only mountains but rivers also. Among the basic local governments in Korea, it ranks second in terms of area after Hongcheon and most of Inje-gun on the 38th parallel belonged to the Democratic People's Republic of Korea . Also the remaining areas were incorporated into Shinnam-myeon and Naeyeon, Hongcheon-gun. After

675-404: Is not a factor used in defining the humid continental climate, snow during the winter in this type of climate is almost a guarantee, either intermittently throughout the winter months near the poleward or coastal margins, or persistently throughout the winter months elsewhere in the climate zone. Humid continental climates are generally found between latitudes 40° N and 60° N , within

720-724: Is noted during the autumn of deciduous forests. In the poleward direction, these climates transition into subarctic climates featuring short summers (and usually very cold winters) allowing only conifer trees. Moving equatorword, the hot-summer continental climates grade into humid subtropical climates (chiefly in North America and Asia) while the warm-summer continental climates grade into oceanic climates (chiefly in Europe), both of which have milder winters where average temperatures stay above 0°C (or -3°C). Some continental climates with lower precipitation (chiefly in Central Asia and

765-597: Is quite cold from early November, with snow falling around its higher peaks. In 2007, the first heavy snow of the year was recorded as early as 16 November. Inje is a modest tourist destination for outdoor activities. It is home to the highest bungee jump in South Korea. It also host the Inje Speedium Resort Circuit. Because of its cold climate, many ice-fishing festivals often occur in Inje and

810-701: Is to be found in northern China including Manchuria and parts of North China , south-east Russia , and over much of the Korean Peninsula ; it has the Köppen classification Dwa . Much of central Asia , northwestern China , and southern Mongolia has a thermal regime similar to that of the Dfa climate type, but these regions receive so little precipitation that they are more often classified as steppes ( BSk ) or deserts ( BWk ). Dsa climates are rare; they are generally restricted to elevated areas adjacent to mid-latitude Mediterranean climate regions with

855-698: The Black Sea coast), Belarus , Russia (mostly central part of European Russia ), south and central parts of the Nordic countries not bathed by the Atlantic Ocean or North Sea : Sweden (historical regions of Svealand and Götaland ), Denmark , Finland (south end, including the three largest cities ), Norway (most populated area), all Baltic States : Estonia , Latvia , Lithuania and also in parts of: Romania (generally above 100 m (328 ft)), Bosnia and Herzegovina , Turkey and in

900-482: The Cairngorm Mountains of Scotland , (generally above 100 m (328 ft)). It has little warming or precipitation effects from the northern Atlantic. The cool summer subtype is marked by mild summers, long cold winters and less precipitation than the hot summer subtype; however, short periods of extreme heat are not uncommon. Northern Japan has a similar climate. In Asia, this climate type

945-484: The Dfa climate type is present near the Black Sea in southern Ukraine , the Southern Federal District of Russia , southern Moldova , Serbia , parts of southern Romania , and Bulgaria , but tends to be drier and can be even semi-arid in these places. In East Asia, this climate exhibits a monsoonal tendency with much higher precipitation in summer than in winter, and due to the effects of

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990-568: The Eight Provinces of Korea during the Joseon Dynasty . The province was formed in 1395, and derived its name from the names of the principal cities of Gangneung (강릉; 江陵) and the provincial capital Wonju (원주; 原州). In 1895, Gangwon-do was replaced by the Districts of Chuncheon ( Chuncheon-bu; 춘천부; 春川府) in the west and Gangneung ( Gangneung-bu; 강릉부; 江陵府) in the east. (Wonju later became part of Chungju District.) In 1896, Korea

1035-538: The Korean Peninsula , parts of Eastern Europe , parts of southern Ontario , much of the American Midwest , and the Northeast US , the climate combines hotter summer maxima and greater humidity (similar to those found in adjacent humid subtropical climates ) and moderately cold winters and more intermittent snow cover (averaging somewhat below freezing, too cold for a more temperate classification), and

1080-591: The Canadian Prairie Provinces and below 40°N in the high Appalachians . In Europe, this subtype reaches its most northerly latitude in Bodø at the 67°N . High-altitude locations such as Flagstaff, Arizona , Aspen, Colorado and Los Alamos, New Mexico in the western United States exhibit local Dfb climates. The south-central and southwestern Prairie Provinces also fits the Dfb criteria from

1125-514: The Korean War, most of the borders of Gangwon-do went north and became Inje-gun, but the inner side was not restored and remained under the jurisdiction of Hongcheon-gun. There are many famous hills, such as Jinbu-ryeong, Misiryeong, Hangyeryeong, Eunbi-ryeong, and Gom-Bae-ryeong. Although it is in the Yeongseo area, it is a point connecting Yeongseo and Yeongdong, so the rent is inevitable. It

1170-787: The UN Forces advanced to the Kansas Line , north of the 38th Parallel . Inje town was lost again to the Chinese People's Volunteer Army during the Fifth Phase Offensive in late April 1951 and was recaptured in the UN May-June 1951 counteroffensive . In 1951 the US Marine Corps 1st Medical Battalion operated a field hospital in Inje town. The 40th Infantry Division assumed responsibility for

1215-547: The Western United States) grade into semi-arid climates with similar temperatures but low precipitation. A hot summer version of a continental climate features an average temperature of at least 22 °C (71.6 °F) in its warmest month. Since these regimes are restricted to the Northern Hemisphere, the warmest month is usually July or August. High temperatures during the warmest month tend to be in

1260-420: The central and northeastern portions of North America , Europe , and Asia . Occasionally, they can also be found at higher elevations above other more temperate climate types. They are rare in the Southern Hemisphere , limited to isolated high altitude locations, due to the larger ocean area at that latitude, smaller land mass, and the consequent greater maritime moderation. In the Northern Hemisphere, some of

1305-459: The classification symbol defines seasonal rainfall as follows: while the third letter denotes the extent of summer heat: Within North America, moisture within this climate regime is supplied by the Great Lakes , Gulf of Mexico and adjacent western subtropical Atlantic . Precipitation is relatively well distributed year-round in many areas with this climate ( f ), while others may see

1350-425: The continents either do not penetrate low enough in latitude or taper too much to have any place that gets the combination of snowy winters and hot summers. Marine influences are very strong around 40°S and such preclude Dfa , Dwa , and Dsa climates from existing in the southern hemisphere. Also known as hemiboreal climate , areas featuring this subtype of the continental climate have an average temperature in

1395-458: The defense of the Kansas Line from the 24th Infantry Division from February 1952 supported by the ROK 3rd Infantry Division . After the war ended, Inje County continued to be a strategic location for the military. The Korea Combat Training Center is located there. The Republic of Korea Army 's III Corps headquarters and its subordinate units are scattered in bases throughout the county. Inje

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1440-779: The end of the Japanese occupation of Korea in 1945, Korea was split into 13 distinctive administrative zones, and Inje County was located in Kangwon Province , and for a short time was under the administration of North Korea. After the Partition of Korea , this historical province was split in half and Inje County fell under the jurisdiction of South Korea. The Republic of Korea Army ROK) 5th Infantry Division recaptured Inje town in Operation Rugged in April 1951 as

1485-518: The front area of Gangwon-do, it is very cold in winter. The average annual temperature is 10,1 °C, the average temperature of January, the coldest month, is -5,2 °C, the average temperature of August, the coldest month is 23,3 °C, and the lowest temperature ever recorded in January 1981 is -25, 9 °C, the highest temperature ever recorded on January is -25,9 °C all-time, 37,7 °C on August 1, 2018. The average annual precipitation

1530-526: The high 20s to low 30s °C (80s °F), while average January afternoon temperatures are near or well below freezing. Frost-free periods typically last 4 to 7 months in this climate regime. Within North America , this climate includes portions of the central and eastern United States from east of 100°W to south of about the 44°N to the Atlantic . Precipitation increases further eastward in this zone and

1575-439: The humid continental climate covers a much larger area than the hot subtype. In North America, the climate zone covers from about 42°N to 50°N latitude mostly east of 100°W , including parts of Southern Ontario , the southern half of Quebec , The Maritimes , and Newfoundland , as well as the northern United States from eastern North Dakota east to Maine . However, it can be found as far north as 54°N , and further west in

1620-474: The humid continental climates, typically in around Hokkaido , Sakhalin Island , northeastern mainland Europe , Scandinavia , Nova Scotia , and Newfoundland are closer to the sea and heavily maritime-influenced and comparable to oceanic climates , with relatively cool summers, significant year-round precipitation (including high amounts of snow) and winters being just below the freezing mark (too cold for such

1665-537: The remnants thereof). Though humidity levels are often high in locations with humid continental climates, the "humid" designation means that the climate is not dry enough to be classified as semi-arid or arid . By definition, forests thrive within this climate. Biomes within this climate regime include temperate woodlands, temperate grasslands, temperate deciduous or evergreen forests, coniferous forests, and coniferous swamps. Within wetter areas, maple , spruce , pine , fir , and oak can be found. Fall foliage

1710-585: The steppe ( BSk ) climates. In the eastern and Midwestern United States, Pennsylvania , Ohio , Illinois , Indiana , southern New York , most of Connecticut and Rhode Island , and eastern Massachusetts fall into the hot-summer humid continental climate. In Canada, this climate type exists only over portions of Southern Ontario . In the Eastern Hemisphere, this climate regime is found within interior Eurasia and east-central Asia. Within Europe,

1755-488: The strong Siberian High much colder winter temperatures than similar latitudes around the world, however with lower snowfall, the exception being western Japan with its heavy snowfall. Tōhoku , between Tokyo and Hokkaidō and Western coast of Japan also has a climate with Köppen classification Dfa , but is wetter even than that part of North America with this climate type. A variant which has dry winters and hence relatively lower snowfall with monsoonal type summer rainfall

1800-435: The warmest month below 22 °C (72 °F). Summer high temperatures in this zone typically average between 21–28 °C (70–82 °F) during the daytime and the average temperatures in the coldest month are generally well or far below the −3 °C (27 °F) (or 0 °C (32.0 °F)) isotherm. Frost-free periods typically last 3–5 months. Heat spells lasting over a week are rare. The warm summer version of

1845-404: The wider Gangwon-do area. However, the ice fishing in Inje is one of the main attractions in winter with 6,000 tourists per weekday and over 10,000 on weekends. 38°04′N 128°10′E  /  38.067°N 128.167°E  / 38.067; 128.167 Gangwon Province (pre-1910) Gangwon Province or Gangwon-do ( Korean pronunciation: [ka̠ŋ.wʌ̹n.do̞] ) was one of

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1890-455: The −3 °C (27 °F) average temperature isotherm (line of equal temperature) was near the southern extent of winter snowpack . In the United States, it is more common to use the 0 °C [32.0 °F] isotherm instead. The 10 °C (50 °F) average temperature was found to be roughly the minimum temperature necessary for tree reproduction and growth. Wide temperature ranges are common within this climate zone. Second letter in

1935-707: Was located in the Soyanggang River basin in the northern region, and its language also uses a Yeongseo dialect similar to Chuncheon. .[8] However, it is difficult to see it as a living area in Chuncheon at present, but the road to go quickly to the construction of the Soyanggang Dam has been submerged, and in the midst of this, the expansion of 44th street has led to active exchanges between Hongcheon - Inje - Sokcho. Expansion Hongcheon - Inje - Sokcho It can be seen as an extended East Seoul living area. Like

1980-475: Was recorded. Think of it as a typical continental climate. Inje has a monsoon-influenced humid continental climate ( Köppen : Dwa ) with cold, dry winters and hot, rainy summers. Daecheong Peak is the highest peak in the Mt. Seorak ranges and is located near at the boundary of Inje county and Yangyang county with an altitude of 1,708m. The beautiful snow scenes around Daecheong peak are widely known. Inje county

2025-642: Was redivided into thirteen provinces, and the two districts were merged to again form Gangwon-do Province. Although Wonju rejoined Gangwon-do province, the provincial capital was moved to Chuncheon (춘천; 春川). With the division of Korea in 1945, the subsequent establishment of separate North and South Korean governments in 1948, and the conclusion of the Korean War in 1953, Gangwon came to be divided into separate provinces once again: Gangwon Province (South Korea) and Kangwon Province (North Korea) . Humid continental climate A humid continental climate

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