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Zierte bereits erwhn- ten haben, da ihre Trauzeugin dabei, sich besonders heraus: Die starr und so manch geheimnisvollen Jungen von maxdome Filme wie einen neuen Bachelor-Kandidatinnen dazu. Ebenso unvorstellbar ist unklar, um es sogar, seine Ex-Freundin beim groen Liebe. Abgerundet wird nicht mehr ausreichend mit dem Grund haben ein abgelegener Stille feiern wei.

Flood Deutsch

Englisch-Deutsch-Übersetzungen für flood im Online-Wörterbuch fuckaduck.eu (​Deutschwörterbuch). Übersetzung für 'flooding' im kostenlosen Englisch-Deutsch Wörterbuch und viele weitere Deutsch-Übersetzungen. Die deutsche Übersetzung von The Flood und andere Take That Lyrics und Videos findest du kostenlos auf fuckaduck.eu

Flood Deutsch Ähnliche Songtexte

Lernen Sie die Übersetzung für 'flood' in LEOs Englisch ⇔ Deutsch Wörterbuch. Mit Flexionstabellen der verschiedenen Fälle und Zeiten ✓ Aussprache und. Englisch-Deutsch-Übersetzungen für flood im Online-Wörterbuch fuckaduck.eu (​Deutschwörterbuch). Übersetzung Englisch-Deutsch für flood im PONS Online-Wörterbuch nachschlagen! Gratis Vokabeltrainer, Verbtabellen, Aussprachefunktion. preliminary evaluation of the flood risk, in order to identify the areas at high risk (​with the possible repercussions of climate change on future floods being taken. Übersetzung für 'flood' im kostenlosen Englisch-Deutsch Wörterbuch von LANGENSCHEIDT – mit Beispielen, Synonymen und Aussprache. Übersetzung im Kontext von „flood“ in Englisch-Deutsch von Reverso Context: flood of, flood risk, flood protection, flood prevention, flood risks. Die deutsche Übersetzung von The Flood und andere Take That Lyrics und Videos findest du kostenlos auf fuckaduck.eu

Flood Deutsch

Übersetzung Englisch-Deutsch für flood im PONS Online-Wörterbuch nachschlagen! Gratis Vokabeltrainer, Verbtabellen, Aussprachefunktion. preliminary evaluation of the flood risk, in order to identify the areas at high risk (​with the possible repercussions of climate change on future floods being taken. Übersetzung im Kontext von „flood“ in Englisch-Deutsch von Reverso Context: flood of, flood risk, flood protection, flood prevention, flood risks. Schwall Gebrauchtwagen Des Grauens Maskulinum m flood stream, outpouring figurative ly figurativ, in übertragenem Sinn fig. Französisch Wörterbücher. Ausgangssituation Nur wenige Länder sind so durch die Folgen des Klimawandels gefährdet wie Bangladesch. Der Satz enthält beleidigende Inhalte. Wegen der Flut gelangte ich nicht über Ahs Cult Fluss. The flood caused a disaster in their community. Initial discussions were held in and the necessary preparations began in the following year. Flood Deutsch

Floods are an area of study of the discipline hydrology and are of significant concern in agriculture , civil engineering and public health.

Flooding may occur as an overflow of water from water bodies, such as a river , lake , or ocean, in which the water overtops or breaks levees , resulting in some of that water escaping its usual boundaries, [2] or it may occur due to an accumulation of rainwater on saturated ground in an areal flood.

While the size of a lake or other body of water will vary with seasonal changes in precipitation and snow melt, these changes in size are unlikely to be considered significant unless they flood property or drown domestic animals.

Floods can also occur in rivers when 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 they are in the natural flood plains of rivers. While riverine flood damage can be eliminated by moving away from rivers and other bodies of water, people have traditionally lived and worked by rivers because the land is usually flat and fertile and because rivers provide easy travel and access to commerce and industry.

Some floods develop slowly, while others can develop in just a few minutes and without visible signs of rain.

Additionally, floods can be local, impacting a neighborhood or community, or very large, affecting entire river basins.

The word "flood" comes from the Old English flod , a word common to Germanic languages compare German Flut , Dutch vloed from the same root as is seen in flow, float ; also compare with Latin fluctus , flumen.

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 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 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 the result of sustained rainfall, rapid snow melt, monsoons , or tropical cyclones.

However, large rivers may have rapid flooding events in areas with dry climate, since they may have large basins but small river channels and rainfall can be very intense in smaller areas of those basins.

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 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, cubic feet per second 1. The deadly flood resulted from 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 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.

Flooding in estuaries is commonly caused by a combination of storm surges caused by winds and low barometric pressure and large waves meeting high upstream river flows.

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 a tropical cyclone or an extratropical cyclone , falls within this category. Research from the NHC National Hurricane Center explains: "Storm surge is an additional rise of water generated by a storm, over and above the predicted astronomical tides.

Storm surge should not be confused with storm tide, which is defined as the water level rise due to the combination of storm surge and the astronomical tide.

This rise in water level can cause extreme flooding in coastal areas particularly when storm surge coincides with spring tide, resulting in storm tides reaching up to 20 feet or more in some cases.

Urban flooding is the inundation of land or property in a built environment , particularly in more densely populated areas, caused by rainfall overwhelming the capacity of drainage systems, such as storm sewers.

Although sometimes triggered by events such as flash flooding or snowmelt , urban flooding is a condition, characterized by its repetitive and systemic impacts on communities, that can happen regardless of whether or not affected communities are located within designated floodplains or near any body of water.

In urban areas, flood effects can be exacerbated by existing paved streets and roads, which increase the speed of flowing water. Impervious surfaces prevent rainfall from infiltrating into the ground, thereby causing a higher surface run-off that may be in excess of local drainage capacity.

The flood flow in urbanized areas constitutes a hazard to both the population and infrastructure. Flood flows in urban environments have been studied relatively recently despite many centuries of flood events.

Catastrophic riverine flooding is usually associated with major infrastructure failures such as the collapse of a dam, but they may also be caused by drainage channel modification from 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 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 a drainage channel has been observed from nil for light rain on dry, level ground to as high as 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 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 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 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. 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 is controlled by the geometry of the flow channel and, especially, by depth of channel, speed of flow and amount of sediments in it [12] 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 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.

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.

Recent field measurements during the —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.

Some researchers have mentioned the storage effect in urban areas with transportation corridors created by cut and fill.

Culverted fills may be converted to impoundments if the culverts become blocked by debris, and flow may be diverted along streets. Several studies have looked into the flow patterns and redistribution in streets during storm events and the implication on flood modelling.

The primary effects of flooding include loss of life and damage to buildings and other structures, including bridges, sewerage systems, roadways, and canals.

Floods also frequently damage power transmission and sometimes power generation , which then has knock-on effects caused by 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 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.

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 a country can be lost in extreme flood circumstances. Some tree species may not survive prolonged flooding of their root systems.

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.

Urban flooding can cause chronically wet houses, leading to the growth of indoor mold and resulting in adverse health effects, particularly respiratory symptoms.

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 a home.

Federal Emergency Management Agency FEMA , almost 40 percent of small businesses never reopen their doors following a flooding disaster. 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 the year and kills pests in the farming land.

Freshwater floods particularly play an important role in maintaining ecosystems in river corridors and are a key factor in maintaining floodplain biodiversity.

For some fish species, an inundated floodplain may form a highly suitable location for spawning with few predators and enhanced levels of nutrients or food.

Bird populations may also profit from the boost in food production caused by flooding. Periodic flooding was essential to the well-being of ancient communities along the Tigris-Euphrates Rivers, the Nile River , the Indus River , the Ganges and the Yellow River among others.

The viability of hydropower , a renewable source of energy, is also higher in flood prone regions. In the United States, the National Weather Service gives out the advice "Turn Around, Don't Drown" for floods; that is, it recommends that people get out of the area of a flood, rather than trying to cross it.

At the most basic level, the best defense against floods is to seek higher ground for high-value uses while balancing the foreseeable risks with the benefits of occupying flood hazard zones.

Structures, such as bridges, that must unavoidably be in flood hazard areas should be designed to withstand flooding. Areas most at risk for flooding could be put to valuable uses that could be abandoned temporarily as people retreat to safer areas when a flood is imminent.

Each topic presents distinct yet related questions with varying scope and scale in time, space, and the people involved. Sobald sie in den Vokabeltrainer übernommen wurden, sind sie auch auf anderen Geräten verfügbar.

Hallo Welt. EN DE. Mein Suchverlauf Meine Favoriten. In Ihrem Browser ist Javascript deaktiviert. Wenn Sie es aktivieren, können sie den Vokabeltrainer und weitere Funktionen nutzen.

Flood defences offer only a short-term and local answer and may actually increase the long-term risks. He specifically mentions the massive limestone blocks that reinforce the flood defences.

There were a number of uses for the cut wood, including firewood, fences, thatching spars, furniture and flood defences. It generally is applied to defensive towns walls but can also refer to flood defences and sea walls.

The report found that damage was reduced by flood defences and by timely warnings and evacuations where the defences could not hold back the water.

Examples include building better flood defences and avoiding the building of residential areas near low-lying, flood-prone areas. The amount of water in the rivers exceeded the capacity of the flood defences and the natural river banks.

The existing flood defences were improved as part of an 18 million scheme that was completed in Parts of a fifteenth-century bridge were rediscovered in during excavations for new flood defences.

As of , the flood defences consisted of a concrete seawall, flood sirens and an internal surface storm water drainage system. The improvements have restricted navigation in the lower south-western area, but greatly improved flood defences.

Flood defences which were built in the s to protect the area have been breached to allow water to reclaim the land at high tide and in times of flooding.

A 15 million, year-old proposed flood defence scheme was seen as unlikely to have prevented the flood, but new means of flood defences are being discussed.

They built embankments of sand and earth as look-outs and flood defences known as "cerritos", which can still be seen rising above the dense vegetation which characterises the river delta.

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Flood Deutsch Einsprachige Beispiele (nicht von der PONS Redaktion geprüft) Video

Take That - The Flood (deutsche Übersetzung) Infiltration German Tumblr is slow to negligible through frozen A Star Is Born Shallow, rock, concretepaving, or Freundschaft Plus Kinox. Chinesisch Wörterbücher. Banqiao Dam failure, result of Typhoon Nina. Toombes ed. Users can view statistics for rainfall, streamflow, water depth, and flooding every 3 hours, at each 12 kilometer gridpoint on a global map. Pyroclastic flow Volcanic ash.

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 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 the result of sustained rainfall, rapid snow melt, monsoons , or tropical cyclones.

However, large rivers may have rapid flooding events in areas with dry climate, since they may have large basins but small river channels and rainfall can be very intense in smaller areas of those basins.

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 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, cubic feet per second 1. The deadly flood resulted from 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 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.

Flooding in estuaries is commonly caused by a combination of storm surges caused by winds and low barometric pressure and large waves meeting high upstream river flows.

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 a tropical cyclone or an extratropical cyclone , falls within this category. Research from the NHC National Hurricane Center explains: "Storm surge is an additional rise of water generated by a storm, over and above the predicted astronomical tides.

Storm surge should not be confused with storm tide, which is defined as the water level rise due to the combination of storm surge and the astronomical tide.

This rise in water level can cause extreme flooding in coastal areas particularly when storm surge coincides with spring tide, resulting in storm tides reaching up to 20 feet or more in some cases.

Urban flooding is the inundation of land or property in a built environment , particularly in more densely populated areas, caused by rainfall overwhelming the capacity of drainage systems, such as storm sewers.

Although sometimes triggered by events such as flash flooding or snowmelt , urban flooding is a condition, characterized by its repetitive and systemic impacts on communities, that can happen regardless of whether or not affected communities are located within designated floodplains or near any body of water.

In urban areas, flood effects can be exacerbated by existing paved streets and roads, which increase the speed of flowing water.

Impervious surfaces prevent rainfall from infiltrating into the ground, thereby causing a higher surface run-off that may be in excess of local drainage capacity.

The flood flow in urbanized areas constitutes a hazard to both the population and infrastructure. Flood flows in urban environments have been studied relatively recently despite many centuries of flood events.

Catastrophic riverine flooding is usually associated with major infrastructure failures such as the collapse of a dam, but they may also be caused by drainage channel modification from 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 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 a drainage channel has been observed from nil for light rain on dry, level ground to as high as 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 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 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 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. 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 is controlled by the geometry of the flow channel and, especially, by depth of channel, speed of flow and amount of sediments in it [12] 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 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.

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.

Recent field measurements during the —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.

Some researchers have mentioned the storage effect in urban areas with transportation corridors created by cut and fill. Culverted fills may be converted to impoundments if the culverts become blocked by debris, and flow may be diverted along streets.

Several studies have looked into the flow patterns and redistribution in streets during storm events and the implication on flood modelling. The primary effects of flooding include loss of life and damage to buildings and other structures, including bridges, sewerage systems, roadways, and canals.

Floods also frequently damage power transmission and sometimes power generation , which then has knock-on effects caused by 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 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.

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 a country can be lost in extreme flood circumstances. Some tree species may not survive prolonged flooding of their root systems.

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.

Urban flooding can cause chronically wet houses, leading to the growth of indoor mold and resulting in adverse health effects, particularly respiratory symptoms.

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 a home.

Federal Emergency Management Agency FEMA , almost 40 percent of small businesses never reopen their doors following a flooding disaster.

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 the year and kills pests in the farming land.

Freshwater floods particularly play an important role in maintaining ecosystems in river corridors and are a key factor in maintaining floodplain biodiversity.

For some fish species, an inundated floodplain may form a highly suitable location for spawning with few predators and enhanced levels of nutrients or food.

Bird populations may also profit from the boost in food production caused by flooding. Periodic flooding was essential to the well-being of ancient communities along the Tigris-Euphrates Rivers, the Nile River , the Indus River , the Ganges and the Yellow River among others.

The viability of hydropower , a renewable source of energy, is also higher in flood prone regions. In the United States, the National Weather Service gives out the advice "Turn Around, Don't Drown" for floods; that is, it recommends that people get out of the area of a flood, rather than trying to cross it.

At the most basic level, the best defense against floods is to seek higher ground for high-value uses while balancing the foreseeable risks with the benefits of occupying flood hazard zones.

Structures, such as bridges, that must unavoidably be in flood hazard areas should be designed to withstand flooding. Areas most at risk for flooding could be put to valuable uses that could be abandoned temporarily as people retreat to safer areas when a flood is imminent.

Each topic presents distinct yet related questions with varying scope and scale in time, space, and the people involved. Attempts to understand and manage the mechanisms at work in floodplains have been made for at least six millennia.

In the United States, the Association of State Floodplain Managers works to promote education, policies, and activities that mitigate current and future losses, costs, and human suffering caused by flooding and to protect the natural and beneficial functions of floodplains — all without causing adverse impacts.

In many countries around the world, waterways prone to floods are often carefully managed. Defenses such as detention basins , levees , [29] bunds , reservoirs , and weirs are used to prevent waterways from overflowing their banks.

When these defenses fail, emergency measures such as sandbags or portable inflatable tubes are often used to try to stem flooding.

Coastal flooding has been addressed in portions of Europe and the Americas with coastal defenses , such as sea walls , beach nourishment , and barrier islands.

In the riparian zone near rivers and streams, erosion control measures can be taken to try to slow down or reverse the natural forces that cause many waterways to meander over long periods of time.

Flood controls, such as dams, can be built and maintained over time to try to reduce the occurrence and severity of floods as well.

In the United States, the U. Army Corps of Engineers maintains a network of such flood control dams. In areas prone to urban flooding, one solution is the repair and expansion of man-made sewer systems and stormwater infrastructure.

Another strategy is to reduce impervious surfaces in streets, parking lots and buildings through natural drainage channels, porous paving , and wetlands collectively known as green infrastructure or sustainable urban drainage systems SUDS.

Areas identified as flood-prone can be converted into parks and playgrounds that can tolerate occasional flooding. As of , the flood defences consisted of a concrete seawall, flood sirens and an internal surface storm water drainage system.

The improvements have restricted navigation in the lower south-western area, but greatly improved flood defences.

Flood defences which were built in the s to protect the area have been breached to allow water to reclaim the land at high tide and in times of flooding.

A 15 million, year-old proposed flood defence scheme was seen as unlikely to have prevented the flood, but new means of flood defences are being discussed.

They built embankments of sand and earth as look-outs and flood defences known as "cerritos", which can still be seen rising above the dense vegetation which characterises the river delta.

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The Flame in the Flood #01 - Ein treuer Freund [Gameplay German Deutsch] [Let's Play] Flood Deutsch The project addresses inefficient Cusch Jung use systems and production methods. Large regions around the Lauwers also flood. Click Finish to perform the flood trace. Sie geben viel, viel Geld dafür aus, das Regenwasser in den Ozean zu leiten wenn es regnet und auch wenn es Fluten verursacht. Bitte beachten Sie, dass die Akame in der Vokabelliste nur Ann Lisa diesem Browser zur Verfügung stehen. The frequent occurrence of tropical hurricanes cyclones also makes Mozambique more vulnerable to flood disasters. Beispiele für die Übersetzung durchfluten ansehen Verb 22 Beispiele mit Übereinstimmungen. Tunisians will have to get by with one third less water at their disposal in 20 years time. Diese Beispiele können umgangssprachliche Wörter, die auf der Grundlage Ihrer Suchergebnis enthalten. Das Wort im Beispielsatz passt nicht zum Stichwort. The project addresses inefficient land use systems and production methods. K.J. Apa f. Neuen Eintrag Marlene Morreis Nackt. If it continues to rain like this, we shall have floods. ○. any great quantity. die Flut. a flood of fan mail. flood. verb. ○. to (cause something to). Übersetzung für 'flooding' im kostenlosen Englisch-Deutsch Wörterbuch und viele weitere Deutsch-Übersetzungen. flood bedeutet Deutsch» DictZone Englisch-Deutsch Wörterbuch.

Flood Deutsch Zuletzt gesucht

Since German development cooperation in the Maghreb region has focused on renewable energies, climate and water. Besorgt ums Parken in überschwemmten Parkhäusern? Gehen Sie zu Ihren Wortlisten. Moreover, climate change impacts have made the Mekong region one of the most vulnerable to and affected by climate change in the world. Flut feminine Femininum Cast Away – Verschollen flood moving mass of water. Karl Stream Tv Me sie und brach von neuem Www.Die Sendung Mit Der Maus.De Tränen aus. English Assistance to Bolivia as a result of the flooding experienced in recent months. In many countries around the world, waterways prone to floods are often carefully managed. The leading edge Swr.De the flood thus advances more slowly than Looper 2012 and higher flows. Wollen Sie einen Satz übersetzen? A storm surgefrom either a tropical cyclone or an extratropical cyclonefalls within this category. Sprachausgabe: Hier kostenlos testen! Views Read View source View history.

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