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Kamo River

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The Kamo River ( 鴨川 , Kamo-gawa , duck river – see onomastics ) is located in Kyoto Prefecture , Japan . The riverbanks are popular walking spots for residents and tourists. In summer, restaurants open balconies looking out to the river. There are walkways running alongside the river, and some stepping stones that cross the river. The water level of the river is usually relatively low; less than one meter in most places. During the rainy season , however, the walkways sometimes flood in their lower stretches.

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75-473: It is known for the two Kamo Shrines on its course: Kamigamo Shrine and Shimogamo Shrine and the shared Chinju no Mori between them Tadasu-no-mori . The Kamo River has its source in the mountains in the area of Mount Sajikigatake , around the boundary of Kumogahata village and Keihoku village in the northern ward of Kyoto. Flowing into the Kyoto Basin from the city area called Kamigamo in

150-449: A dam , landslide, or glacier . In one instance, a flash flood killed eight people enjoying the water on a Sunday afternoon at a popular waterfall in a narrow canyon. Without any observed rainfall, the flow rate increased from about 50 to 1,500 cubic feet per second (1.4 to 42 m /s) in just one minute. Two larger floods occurred at the same site within a week, but no one was at the waterfall on those days. The deadly flood resulted from

225-646: A flash flood . Flash floods usually result from intense rainfall over a relatively small area, or if the area was already saturated from previous precipitation. The amount, location, and timing of water reaching a drainage channel from natural precipitation and controlled or uncontrolled reservoir releases determines the flow at downstream locations. Some precipitation evaporates, some slowly percolates through soil, some may be temporarily sequestered as snow or ice, and some may produce rapid runoff from surfaces including rock, pavement, roofs, and saturated or frozen ground. The fraction of incident precipitation promptly reaching

300-515: A landslide , earthquake or volcanic eruption . Examples include outburst floods and lahars . Tsunamis can cause catastrophic coastal flooding , most commonly resulting from undersea earthquakes. The primary effects of flooding include loss of life and damage to buildings and other structures, including bridges, sewerage systems, roadways, and canals. The economic impacts caused by flooding can be severe. Every year flooding causes countries billions of dollars worth of damage that threatens

375-484: A tropical cyclone or an extratropical cyclone , falls within this category. A storm surge is "an additional rise of water generated by a storm, over and above the predicted astronomical tides". Due to the effects of climate change (e.g. sea level rise and an increase in extreme weather events) and an increase in the population living in coastal areas, the damage caused by coastal flood events has intensified and more people are being affected. Flooding in estuaries

450-468: A country can be lost in extreme flood circumstances. Some tree species may not survive prolonged flooding of their root systems. Flooding in areas where people live also has significant economic implications for affected neighborhoods. In the United States , industry experts estimate that wet basements can lower property values by 10–25 percent and are cited among the top reasons for not purchasing

525-538: A drainage channel has been observed from nil for light rain on dry, level ground to as high as 170 percent for warm rain on accumulated snow. Most precipitation records are based on a measured depth of water received within a fixed time interval. Frequency of a precipitation threshold of interest may be determined from the number of measurements exceeding that threshold value within the total time period for which observations are available. Individual data points are converted to intensity by dividing each measured depth by

600-627: A few minutes for roof and parking lot drainage structures, while cumulative rainfall over several days would be critical for river basins. Water flowing downhill ultimately encounters downstream conditions slowing movement. The final limitation in coastal flooding lands is often the ocean or some coastal flooding bars which form natural lakes . In flooding low lands, elevation changes such as tidal fluctuations are significant determinants of coastal and estuarine flooding. Less predictable events like tsunamis and storm surges may also cause elevation changes in large bodies of water. Elevation of flowing water

675-605: A few. Gastrointestinal disease and diarrheal diseases are very common due to a lack of clean water during a flood. Most of clean water supplies are contaminated when flooding occurs. Hepatitis A and E are common because of the lack of sanitation in the water and in living quarters depending on where the flood is and how prepared the community is for a flood. When floods hit, people lose nearly all their crops, livestock, and food reserves and face starvation. Floods also frequently damage power transmission and sometimes power generation , which then has knock-on effects caused by

750-508: A history which pre-dates the founding of Japan's ancient capital. Although now incorporated within boundaries of the city, the Tadasu no Mori location was a site planning factor. It is theorized that this forest was the primeval forest home of the sacerdotal Kamo clan, who were the exclusive caretakers of the shrine from prehistoric times. The boundaries of today's smaller forest encompasses approximately 12.4 hectares, which are preserved as

825-728: A home. According to the U.S. Federal Emergency Management Agency (FEMA), almost 40 percent of small businesses never reopen their doors following a flooding disaster. In the United States, insurance is available against flood damage to both homes and businesses. Economic hardship due to a temporary decline in tourism, rebuilding costs, or food shortages leading to price increases is a common after-effect of severe flooding. The impact on those affected may cause psychological damage to those affected, in particular where deaths, serious injuries and loss of property occur. Fatalities connected directly to floods are usually caused by drowning ;

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900-486: A more distant point controls at higher water levels. Effective flood channel geometry may be changed by growth of vegetation, accumulation of ice or debris, or construction of bridges, buildings, or levees within the flood channel. Periodic floods occur on many rivers, forming a surrounding region known as the flood plain . Even when rainfall is relatively light, the shorelines of lakes and bays can be flooded by severe winds—such as during hurricanes —that blow water into

975-408: A national historical site (を国の史跡). The woods of this sacred grove are designated by UNESCO as a World Cultural Heritage site along with other Shinto shrines in its environs. The shrine's annual festival, Kamo no Matsuri , also called Aoi Matsuri , is the oldest of Kyoto's three major festivals. The others are Jidai Matsuri and Gion Matsuri . The popular name for Kamo-wakeikazuchi jinja

1050-413: A thunderstorm over part of the drainage basin, where steep, bare rock slopes are common and the thin soil was already saturated. Flash floods are the most common flood type in normally-dry channels in arid zones, known as arroyos in the southwest United States and many other names elsewhere. In that setting, the first flood water to arrive is depleted as it wets the sandy stream bed. The leading edge of

1125-520: A type of hybrid river/areal flooding can occur, known locally as "overland flooding". This is different from "overland flow" defined as "surface runoff". The Red River Valley is a former glacial lakebed, created by Lake Agassiz , and over a length of 550 mi (890 km), the river course drops only 236 ft (72 m), for an average slope of about 5 inches per mile (or 8.2 cm per kilometer). In this very large area, spring snowmelt happens at different rates in different places, and if winter snowfall

1200-460: Is a general term for an important Shinto sanctuary complex on both banks of the Kamo River in northeast Kyoto . It is centered on two shrines. The two shrines, an upper and a lower, lie in a corner of the old capital which was known as the "devil's gate" ( 鬼門 , kimon ) due to traditional geomancy beliefs that the north-east corner brought misfortune. Because the Kamo River runs from

1275-419: Is also the birthplace of Kabuki . In 1603 Izumo no Okuni formed a troupe of female dancers and began performing on a makeshift stage, on the dry bed of the river. [REDACTED] Media related to Kamo River at Wikimedia Commons 34°55′53″N 135°44′14″E  /  34.931416°N 135.737236°E  / 34.931416; 135.737236 Kamo Shrines Kamo Shrine ( 賀茂神社 , Kamo-jinja )

1350-405: Is also the intentional flooding of land that would otherwise remain dry. This may take place for agricultural, military, or river-management purposes. For example, agricultural flooding may occur in preparing paddy fields for the growing of semi-aquatic rice in many countries. Flooding may occur as an overflow of water from water bodies, such as a river , lake , sea or ocean. In these cases,

1425-419: Is common when heavy flows move uprooted woody vegetation and flood-damaged structures and vehicles, including boats and railway equipment. Recent field measurements during the 2010–11 Queensland floods showed that any criterion solely based upon the flow velocity, water depth or specific momentum cannot account for the hazards caused by velocity and water depth fluctuations. These considerations ignore further

1500-493: Is commonly caused by a combination of storm surges caused by winds and low barometric pressure and large waves meeting high upstream river flows. The intentional flooding of land that would otherwise remain dry may take place for agricultural, military or river-management purposes. This is a form of hydraulic engineering . Agricultural flooding may occur in preparing paddy fields for the growing of semi-aquatic rice in many countries. Flooding for river management may occur in

1575-400: Is controlled by the geometry of the flow channel and, especially, by depth of channel, speed of flow and amount of sediments in it Flow channel restrictions like bridges and canyons tend to control water elevation above the restriction. The actual control point for any given reach of the drainage may change with changing water elevation, so a closer point may control for lower water levels until

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1650-470: Is left to grow in its natural state. It is neither planted nor pruned. Although Kamigamo and Shimogamo shrines are considered to be paired or twinned, they are not located next to each other. Approximately 2 km. distance separates these two Shinto shrine complexes, which can be explained in part because shrines on the outskirts of Heian-kyō were developed to prevent the infiltration of demons. The Kamogawa river descends from an ill-omened direction; and

1725-461: Is more significant to flooding within small drainage basins. The most important upslope factor in determining flood magnitude is the land area of the watershed upstream of the area of interest. Rainfall intensity is the second most important factor for watersheds of less than approximately 30 square miles or 80 square kilometres. The main channel slope is the second most important factor for larger watersheds. Channel slope and rainfall intensity become

1800-571: Is the Kamigamo jinja or Kamigamo Shrine , also called Upper Shrine. In part, it is called the "upper" shrine because it is situated on the east bank of the Kamo River ( 鴨川 or 賀茂川 , Kamo-gawa ) up-stream from its non-identical twin. The more commonly used name for Kamo-mioya jinja is the Shimogamo jinja or Shimogamo Shrine , also called the Lower Shrine. In part, it is called

1875-454: Is the father of Kamo Taayori-hime. All feature prominently in the annual Aoi Festival , which occurs in May. Featured in this event are a procession between the two shrines, horse races, and demonstrations of mounted archery ( yabusame ). Kamigamo Shrine's two large conical sand mounds memorialize the holy trees that once served to welcome spirits. Shimogama Shrine has since become one of

1950-834: The Horikawa River and West Takase River join with it, and at Shimomukōjima-cho in the Shimotoba part of Fushimi Ward of Kyoto City, it joins with the Katsura River , to become a tributary of the Yodo River . There is a theory that in former times the main stream of the Kamo River was along the Horikawa river about 1 kilometre (1 mile) north of Misono Bridge , and when the Heian Capital (now Kyoto)

2025-562: The Second World War ). Floods are caused by many factors or a combination of any of these generally prolonged heavy rainfall (locally concentrated or throughout a catchment area), highly accelerated snowmelt , severe winds over water, unusual high tides, tsunamis , or failure of dams, levees , retention ponds , or other structures that retained the water. Flooding can be exacerbated by increased amounts of impervious surface or by other natural hazards such as wildfires, which reduce

2100-562: The water table is shallow, such as a floodplain , or from intense rain from one or a series of storms . Infiltration also is slow to negligible through frozen ground, rock, concrete , paving, or roofs. Areal flooding begins in flat areas like floodplains and in local depressions not connected to a stream channel, because the velocity of overland flow depends on the surface slope. Endorheic basins may experience areal flooding during periods when precipitation exceeds evaporation. Floods occur in all types of river and stream channels, from

2175-685: The " Historic Monuments of Ancient Kyoto " which have been designated by UNESCO as a World Heritage Site . The jinja name identifies the clustered kami or deities who are venerated at the Kamo Shrine; and the name refers to the ambit of shrine's encircling woods. The shrine name also references the area's early inhabitants, the Kamo clan , many of whom continue to live near the shrine their ancestors traditionally served. The Kamo are credited with establishing this Shinto sacred place. The formal names of corollary jinja memorialize vital roots in

2250-533: The "lower" shrine because it is situated at the confluence of the Takano River ( 高野川 , Takano-gawa ) and the Kamo River down-stream from its twin. The Kamo Shrine is so named because its rituals and festivals are designed to assist in the veneration of the Kamo family of kami and other associated deities; and Kamo kami ( kami-no-Kamo ) is referenced in other Shinto contexts. In the "Congratulatory Words of

2325-526: The 19th day of the 6th month of 815 in the history Nihonkiryaku (日本記略), it is referred to as 鴨川. Now, the river north of where it joins with the Takano River is usually distinguished as the 加茂川 when written in kanji, and the river south of there is distinguished as the 鴨川. The geographical area called Kamigamo, around the mouth of the valley leading into the Kyoto Basin, became the home grounds of

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2400-536: The Chieftain of Izumo," the "sacred grove of Kamo" is mentioned along with other wooded Shinto sanctuaries at Ō-miwa , Unade and Asuka : At the Kamigamo Shrine, Kamo Wake-ikazuchi , the kami of thunder, is the focus of attention and reverence. Shimogamo Shrine is dedicated to the veneration of Kamo Wake-ikazuchi's mother, Kamo Tamayori-hime . Shimogamo is also dedicated to Kamo Taketsune , who

2475-595: The Kamo (賀茂) clan in ancient times. From this, there arose the regional name Otagi Region Kamo Block (愛宕郡賀茂郷), and consequently the geographical name Kamo (賀茂) set down roots. The river name took after this geographical name. From the Deai Bridge until the Iwaya Bridge north of Kyoto city it is called Kumogahatagawa (雲が畑川) as it passes through the Kumogahata village. North of the Iwaya Bridge until its source

2550-414: The Kamo River is known as Ojitanigawa (祖父谷川). When the palace at the new Heian Capital (now Kyoto) was constructed at the end of the 8th century, the river's course was altered to flow east of the palace. Floods often threatened the ancient capital. Emperor Shirakawa recited his three unmanageable things: Sōhei (armed monks of Enryaku-ji ), dice, and the water of the Kamo River. These days, however,

2625-487: The Kamo Shrine. These heihaku were initially presented to 16 shrines. The lower shrine is that of a kami mother; and the upper shrine is that of her kami offspring. The head priests of both have the same title, Kamo-no-Agata-no Nushi. In agata-no-nushi titles, the appended noun is typically a place name; but in a Taihō ritsuryō consolidation, the Kamo mirror the Yamato clan 's amalgamating conventions in merging

2700-597: The Nishimura House, is open to the public. The Shimogamo Shrine was officially designated Kanpei-taisha in 1871. Shimogamo Shrine is believed to be 100 years older than Kamigamo Shrine, dating back to the 6th century. A shrine structure was erected in 678 during the reign of the Emperor Tenmu , and this became the principal building during the reign or of the Emperor Kanmu when he transferred

2775-717: The adverse ecological impact of the inundation. That impact may also be adverse in a hydrogeological sense if the inundation lasts a long time. Examples for uncontrolled inundations are the second Siege of Leiden during the first part of the Eighty Years' War , the flooding of the Yser plain during the First World War , and the Inundation of Walcheren , and the Inundation of the Wieringermeer during

2850-423: The amount of water damage and mold that grows after an incident. Research suggests that there will be an increase of 30–50% in adverse respiratory health outcomes caused by dampness and mold exposure for those living in coastal and wetland areas. Fungal contamination in homes is associated with increased allergic rhinitis and asthma. Vector borne diseases increase as well due to the increase in still water after

2925-498: The area, its name, its sacred centers and its kami within a single nominative identifier. From 1871 through 1946, the Kamigamo Shrine was officially designated one of the Kanpei-taisha ( 官幣大社 ) , meaning that it stood in the first rank of government supported shrines. It is famous for its haiden (worship hall), rebuilt in 1628-1629 ( Kan'ei 6 ). A number of priests' residences are situated on its grounds, and one,

3000-421: The capital from Heijō-kyō , and Nagaoka-kyō to Heian-kyō . Flood A flood is an overflow of water ( or rarely other fluids ) that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide . Floods are of significant concern in agriculture , civil engineering and public health . Human changes to the environment often increase

3075-434: The deadliest floods worldwide, showing events with death tolls at or above 100,000 individuals. Floods (in particular more frequent or smaller floods) can also bring many benefits, such as recharging ground water , making soil more fertile and increasing nutrients in some soils. Flood waters provide much needed water resources in arid and semi-arid regions where precipitation can be very unevenly distributed throughout

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3150-576: The field that is intended to impede the movement of the enemy. This may be done both for offensive and defensive purposes. Furthermore, in so far as the methods used are a form of hydraulic engineering, it may be useful to differentiate between controlled inundations and uncontrolled ones. Examples for controlled inundations include those in the Netherlands under the Dutch Republic and its successor states in that area and exemplified in

3225-470: The flood process; before, during and after. During floods accidents occur with falling debris or any of the many fast moving objects in the water. After the flood rescue attempts are where large numbers injuries can occur. Communicable diseases are increased due to many pathogens and bacteria that are being transported by the water .There are many waterborne diseases such as cholera , hepatitis A , hepatitis E and diarrheal diseases , to mention

3300-492: The flood thus advances more slowly than later and higher flows. As a result, the rising limb of the hydrograph becomes ever quicker as the flood moves downstream, until the flow rate is so great that the depletion by wetting soil becomes insignificant. Coastal areas may be flooded by storm surges combining with high tides and large wave events at sea, resulting in waves over-topping flood defenses or in severe cases by tsunami or tropical cyclones. A storm surge , from either

3375-403: The floods have settled. The diseases that are vector borne are malaria , dengue , West Nile , and yellow fever . Floods have a huge impact on victims' psychosocial integrity . People suffer from a wide variety of losses and stress . One of the most treated illness in long-term health problems are depression caused by the flood and all the tragedy that flows with one. Below is a list of

3450-428: The flow rate exceeds the capacity of the river channel , particularly at bends or meanders in the waterway . Floods often cause damage to homes and businesses if these buildings are in the natural flood plains of rivers. People could avoid riverine flood damage by moving away from rivers. However, people in many countries have traditionally lived and worked by rivers because the land is usually flat and fertile . Also,

3525-483: The forested area, Tadasu-no-mori . In Japanese the river is called Kamo-gawa , officially written using the kanji compound 鴨川. The first kanji means "wild duck" and is read kamo , and the second kanji means "river" and is read gawa . However, other kanji applied to this name are 賀茂川 or 加茂川. The first appearance in historical documents of the kanji 賀茂川 is in the Yamashiro no kuni fudoki (山城国風土記). In an entry dated

3600-656: The form of diverting flood waters in a river at flood stage upstream from areas that are considered more valuable than the areas that are sacrificed in this way. This may be done ad hoc , or permanently, as in the so-called overlaten (literally "let-overs"), an intentionally lowered segment in Dutch riparian levees, like the Beerse Overlaat in the left levee of the Meuse between the villages of Gassel and Linden, North Brabant . Military inundation creates an obstacle in

3675-774: The intensity and frequency of flooding. Examples for human changes are land use changes such as deforestation and removal of wetlands , changes in waterway course or flood controls such as with levees . Global environmental issues also influence causes of floods, namely climate change which causes an intensification of the water cycle and sea level rise . For example, climate change makes extreme weather events more frequent and stronger. This leads to more intense floods and increased flood risk. Natural types of floods include river flooding, groundwater flooding coastal flooding and urban flooding sometimes known as flash flooding. Tidal flooding may include elements of both river and coastal flooding processes in estuary areas. There

3750-453: The key shrines in the area, being associated with prayers to ensure the success of the annual rice harvest. The Shrine is located within Tadasu no Mori (糺の森), 'the forest of truth,' a primeval forest that is reputed to have never been burned down. The forest has, in fact, suffered some damage over the centuries when all of Kyoto was burned during successive revolts and wars; but the forest growth has rebounded again and again. Tadasu no mori

3825-482: The land for the capital. The city was laid with its northernmost boundary at the present confluence of the Kamo and Takano rivers (just south of today's Imadegawa Street )." The riverbanks where the Kamo River and Takano River join are known as the Tadasu River Banks (Jp., Tadasu-gawara 糺河原). At the triangular area of land here, there is the "River Confluence" shrine of Shimogamo Shrine , which leads into

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3900-403: The land in quantities that cannot be carried within stream channels or retained in natural ponds, lakes, and human-made reservoirs . About 30 percent of all precipitation becomes runoff and that amount might be increased by water from melting snow. River flooding is often caused by heavy rain, sometimes increased by melting snow. A flood that rises rapidly, with little or no warning, is called

3975-614: The livelihood of individuals. As a result, there is also significant socio-economic threats to vulnerable populations around the world from flooding. For example, in Bangladesh in 2007, a flood was responsible for the destruction of more than one million houses. And yearly in the United States, floods cause over $ 7 billion in damage. Flood waters typically inundate farm land, making the land unworkable and preventing crops from being planted or harvested, which can lead to shortages of food both for humans and farm animals. Entire harvests for

4050-417: The location of the flood. Damage to roads and transport infrastructure may make it difficult to mobilize aid to those affected or to provide emergency health treatment. Flooding can cause chronically wet houses, leading to the growth of indoor mold and resulting in adverse health effects, particularly respiratory symptoms. Respiratory diseases are a common after the disaster has occurred. This depends on

4125-436: The loss of power. This includes loss of drinking water treatment and water supply, which may result in loss of drinking water or severe water contamination. It may also cause the loss of sewage disposal facilities. Lack of clean water combined with human sewage in the flood waters raises the risk of waterborne diseases , which can include typhoid , giardia , cryptosporidium , cholera and many other diseases depending upon

4200-619: The north-east direction into the city, the two shrines along the river were intended to prevent demons from entering the city. The Kamo Shrine encompasses what are now independent but traditionally associated jinja or shrines: the Kamo-wakeikazuchi Shrine ( 賀茂別雷神社 , Kamo-wakeikazuchi jinja ) in Kyoto's Kita Ward, and the "Kamo-mioya Shrine'" ( 賀茂御祖神社 , Kamo-mioya jinja ) in Sakyo Ward. They are amongst

4275-457: The period of time between observations. This intensity will be less than the actual peak intensity if the duration of the rainfall event was less than the fixed time interval for which measurements are reported. Convective precipitation events (thunderstorms) tend to produce shorter duration storm events than orographic precipitation. Duration, intensity, and frequency of rainfall events are important to flood prediction. Short duration precipitation

4350-586: The result of sustained rainfall, rapid snow melt, monsoons , or tropical cyclones . However, large rivers may have rapid flooding events in areas with dry climates, since they may have large basins but small river channels, and rainfall can be very intense in smaller areas of those basins. In extremely flat areas, such as the Red River Valley of the North in Minnesota , North Dakota , and Manitoba ,

4425-480: The risks associated with large debris entrained by the flow motion. Floods can be a huge destructive power. When water flows, it has the ability to demolish all kinds of buildings and objects, such as bridges, structures, houses, trees, and cars. Economical, social and natural environmental damages are common factors that are impacted by flooding events and the impacts that flooding has on these areas can be catastrophic. There have been numerous flood incidents around

4500-599: The river is a famous legend set in the late Heian period . Sanjō Bridge was regarded as the west end of the Tōkaidō during the Edo period . In the past, the river was a crucial source of relatively pure drinking water for Kyoto residents. It also played a role in Kyo-Yuzen dyeing, a famous craft of Kyoto. The river is also the source of the stone that is a glaze ingredient used in traditional Japanese raku pottery. The Kamo River

4575-468: The riverbanks are reinforced with concrete and have improved drainage systems. The merchant Suminokura Ryōi constructed the Takase River on a parallel with the Kamo River in early 17th century. Transportation was done on the canal instead of the unstable mainstream. The encounter between Minamoto no Yoshitsune and Benkei at Gojō Bridge (not the present one, but presumably Matsubara Bridge) over

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4650-454: The rivers provide easy travel and access to commerce and industry. Flooding can damage property and also lead to secondary impacts. These include in the short term an increased spread of waterborne diseases and vector-bourne disesases , for example those diseases transmitted by mosquitos. Flooding can also lead to long-term displacement of residents. Floods are an area of study of hydrology and hydraulic engineering . A large amount of

4725-628: The same northern ward of the city, from there it bends south-east and, around the spot known as Demachi in the Kamigyō (or "Upper Kyoto" ward), joins with the Takano River which flows down from the northeastern direction, and there changes direction to due south through Kyoto's Nakagyō ("Central") ward. In the vicinity of the Shijō Bridge at Shijō Street in the center of downtown Kyoto, the Shirakawa River joins with it. At its southern part,

4800-497: The shore areas. Extreme flood events often result from coincidence such as unusually intense, warm rainfall melting heavy snow pack, producing channel obstructions from floating ice, and releasing small impoundments like beaver dams. Coincident events may cause extensive flooding to be more frequent than anticipated from simplistic statistical prediction models considering only precipitation runoff flowing within unobstructed drainage channels. Debris modification of channel geometry

4875-531: The shrines along the flow were positioned in order to prevent demons from using the river to enter the city. Although Kamo-jinja is not directly on the banks of the Kamo River, the site locations were positioned as part of a plan for mitigating the consequences of periodic flooding. The shrines became the object of Imperial patronage during the early Heian period . In 965, Emperor Murakami ordered that Imperial messengers were sent to report important events to Japan's guardian kami, including those venerated at

4950-538: The smallest ephemeral streams in humid zones to normally-dry channels in arid climates to the world's largest rivers. When overland flow occurs on tilled fields, it can result in a muddy flood where sediments are picked up by run off and carried as suspended matter or bed load . Localized flooding may be caused or exacerbated by drainage obstructions such as landslides , ice , debris , or beaver dams. Slow-rising floods most commonly occur in large rivers with large catchment areas . The increase in flow may be

5025-527: The supply of vegetation that can absorb rainfall. During times of rain, some of the water is retained in ponds or soil, some is absorbed by grass and vegetation, some evaporates, and the rest travels over the land as surface runoff . Floods occur when ponds, lakes, riverbeds, soil, and vegetation cannot absorb all the water. This has been exacerbated by human activities such as draining wetlands that naturally store large amounts of water and building paved surfaces that do not absorb any water. Water then runs off

5100-440: The third most important factors for small and large watersheds, respectively. Time of Concentration is the time required for runoff from the most distant point of the upstream drainage area to reach the point of the drainage channel controlling flooding of the area of interest. The time of concentration defines the critical duration of peak rainfall for the area of interest. The critical duration of intense rainfall might be only

5175-699: The two Hollandic Water Lines , the Stelling van Amsterdam , the Frisian Water Line , the IJssel Line , the Peel-Raam Line , and the Grebbe line in that country. To count as controlled , a military inundation has to take the interests of the civilian population into account, by allowing them a timely evacuation , by making the inundation reversible , and by making an attempt to minimize

5250-487: The water overtops or breaks levees , resulting in some of that water escaping its usual boundaries. Flooding may also occur due to an accumulation of rainwater on saturated ground. This is called an areal flood . The size of a lake or other body of water naturally varies with seasonal changes in precipitation and snow melt. Those changes in size are however not considered a flood unless they flood property or drown domestic animals . Floods can also occur in rivers when

5325-515: The waters in a flood are very deep and have strong currents . Deaths do not just occur from drowning, deaths are connected with dehydration , heat stroke , heart attack and any other illness that needs medical supplies that cannot be delivered. Injuries can lead to an excessive amount of morbidity when a flood occurs. Injuries are not isolated to just those who were directly in the flood, rescue teams and even people delivering supplies can sustain an injury. Injuries can occur anytime during

5400-450: The world which have caused devastating damage to infrastructure, the natural environment and human life. Floods can have devastating impacts to human societies. Flooding events worldwide are increasing in frequency and severity, leading to increasing costs to societies. Catastrophic riverine flooding can result from major infrastructure failures, often the collapse of a dam . It can also be caused by drainage channel modification from

5475-557: The world's population lives in close proximity to major coastlines , while many major cities and agricultural areas are located near floodplains . There is significant risk for increased coastal and fluvial flooding due to changing climatic conditions. Floods can happen on flat or low-lying areas when water is supplied by rainfall or snowmelt more rapidly than it can either infiltrate or run off . The excess accumulates in place, sometimes to hazardous depths. Surface soil can become saturated, which effectively stops infiltration, where

5550-490: Was established, the river was diverted to its present route. According to historian Herbert E. Plutschow , "To allow a river to flow through and thereby divide a capital would have symbolized potential disunity of the nation. One of the first tasks, therefore, in laying out the new capital was to divert the rivers. The Kamo River once flowed through what is now Horikawa Street and met the Takano River south of their present confluence. Thus, large-scale works were required to prepare

5625-765: Was heavy, a fast snowmelt can push water out of the banks of a tributary river so that it moves overland, to a point further downstream in the river or completely to another streambed. Overland flooding can be devastating because it is unpredictable, it can occur very suddenly with surprising speed, and in such flat land it can run for miles. It is these qualities that set it apart from simple "overland flow". Rapid flooding events, including flash floods , more often occur on smaller rivers, rivers with steep valleys, rivers that flow for much of their length over impermeable terrain, or normally-dry channels. The cause may be localized convective precipitation (intense thunderstorms ) or sudden release from an upstream impoundment created behind

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