Causes of Droughts

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Match the atmospheric changes with their potential effects on precipitation patterns:

Shifts in high and low-pressure systems = More frequent or severe droughts Changes in wind patterns = Altered precipitation patterns Global warming = Increased evaporation rates Movement of jet streams = Blockage of moist air masses

Match the factors that influence rainfall patterns with their descriptions:

Land-Sea Interactions = Blockage of moist air masses by mountains Local and Regional Factors = Influence of sea surface temperatures and ocean currents Atmospheric Changes = Effect of topography and vegetation cover Global Warming = Changes in wind patterns and precipitation

Match the components of the atmosphere with their roles in precipitation:

Moist air masses = Leading to dry conditions on the leeward side Ocean currents = Influencing the amount of moisture available Sea surface temperatures = Affecting evaporation rates Jet streams = Shifting high and low-pressure systems

Match the effects of warmer sea surface temperatures with their consequences on rainfall:

Increased evaporation rates = Enhancing rainfall in some regions Reduced moisture = Contributing to drought conditions Changes in wind patterns = Altering precipitation patterns Blockage of moist air masses = Leading to dry conditions on the leeward side

Match the regional factors with their influences on rainfall variability:

Topography = Blocking moist air masses Vegetation cover = Affecting soil moisture Soil moisture = Influencing evaporation rates Mountains = Causing rain to fall on one side and leading to dry conditions on the other

Match the atmospheric changes with their potential causes:

Changes in wind patterns = Global warming Shifts in high and low-pressure systems = Local and regional factors Movement of jet streams = Land-Sea Interactions Global warming = Atmospheric changes

Match the factors that influence moisture availability with their descriptions:

Sea surface temperatures = Influencing evaporation rates Ocean currents = Affecting precipitation patterns Soil moisture = Blocking moist air masses Vegetation cover = Influencing the amount of moisture available

Match the consequences of drought conditions with their causes:

Reduced moisture = Warmer sea surface temperatures Altered precipitation patterns = Global warming Dry conditions on the leeward side = Local and regional factors Increased evaporation rates = Changes in wind patterns

Match the following factors with their effects on drought:

Variability in Rainfall = Reduces rainfall in South Asia and Australia Global Climate Change = Increases rainfall in parts of South America Deforestation = Alters the distribution and amount of rainfall in various regions Overuse of Water = Changes weather conditions across the globe

Match the following climatic patterns with their effects on rainfall:

El Niño-Southern Oscillation (ENSO) = Increases rainfall in parts of South America North Atlantic Oscillation (NAO) = Reduces rainfall in South Asia and Australia Indian Ocean Dipole (IOD) = Changes weather conditions across the globe Atmospheric Circulation = Alters the distribution and amount of rainfall in various regions

Match the following human activities with their effects on drought:

Deforestation = Changes weather conditions across the globe Overuse of Water = Reduces rainfall in South Asia and Australia Land Degradation = Alters the distribution and amount of rainfall in various regions Global Climate Change = Increases rainfall in parts of South America

Match the following effects on drought with their causes:

Changes weather conditions across the globe = Global Climate Change Alters the distribution and amount of rainfall in various regions = Variability in Rainfall Reduces rainfall in South Asia and Australia = El Niño-Southern Oscillation (ENSO) Increases rainfall in parts of South America = Atmospheric Circulation

Match the following factors with their effects on rainfall distribution:

El Niño-Southern Oscillation (ENSO) = Reduces rainfall in South Asia and Australia Variability in Rainfall = Changes weather conditions across the globe Atmospheric Circulation = Alters the distribution and amount of rainfall in various regions Global Climate Change = Increases rainfall in parts of South America

Match the following factors with their effects on weather conditions:

Global Climate Change = Changes weather conditions across the globe Deforestation = Alters the distribution and amount of rainfall in various regions Land Degradation = Reduces rainfall in South Asia and Australia Overuse of Water = Increases rainfall in parts of South America

Match the following effects on drought with their causes:

Alters the distribution and amount of rainfall in various regions = Atmospheric Circulation Changes weather conditions across the globe = Global Climate Change Reduces rainfall in South Asia and Australia = Deforestation Increases rainfall in parts of South America = Variability in Rainfall

Match the following climatic patterns with their effects on drought:

Indian Ocean Dipole (IOD) = Changes weather conditions across the globe North Atlantic Oscillation (NAO) = Reduces rainfall in South Asia and Australia El Niño-Southern Oscillation (ENSO) = Increases rainfall in parts of South America Atmospheric Circulation = Alters the distribution and amount of rainfall in various regions

Study Notes

Drought Causes

  • Droughts are caused by a combination of natural weather patterns and human activities.
  • Variability in rainfall, global climate change, deforestation, overuse of water, and land degradation are the main factors contributing to droughts.

Variability in Rainfall

  • Variability in rainfall is closely tied to large-scale climatic patterns and systems, such as El Niño-Southern Oscillation (ENSO), North Atlantic Oscillation (NAO), and Indian Ocean Dipole (IOD).
  • These patterns can significantly influence weather conditions across the globe, altering the distribution and amount of rainfall in various regions.
  • For example, El Niño events typically reduce rainfall in South Asia and Australia, leading to drought conditions, while increasing it in parts of South America.

Atmospheric Circulation

  • Changes in atmospheric circulation can also cause variability in rainfall.
  • The movement of jet streams, shifts in high and low-pressure systems, and changes in wind patterns can all affect where and how much rain falls.
  • These atmospheric changes can be influenced by global warming and other climatic shifts, leading to altered precipitation patterns and potentially more frequent or severe droughts.

Land-Sea Interactions

  • The interactions between land and sea significantly affect rainfall patterns.
  • Sea surface temperatures, ocean currents, and coastal upwelling can influence the amount of moisture available in the atmosphere, which in turn affects precipitation patterns.
  • Warmer sea surface temperatures can increase evaporation rates, potentially enhancing rainfall in some regions while diminishing it in others, contributing to drought conditions where the moisture is reduced.

Local and Regional Factors

  • Local and regional factors, such as topography, vegetation cover, and soil moisture, can also influence rainfall variability.
  • Mountains can block moist air masses, causing rain to fall on one side (windward) and leading to dry conditions on the other (leeward).
  • Similarly, areas with dense vegetation can increase evapotranspiration, leading to reduced rainfall in those regions.

Droughts are caused by a combination of natural weather patterns and human activities. Learn about the main factors contributing to droughts, including variability in rainfall, global climate change, and more.

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