Short Term Changes To The Water Cycle Flashcards
What’s monitored
Close monitoring through satellite technology and remote sensing
Global air temps, sea surface temps, sea ice thickness, rates of deforestation
Diurnal changes
Within 24 hours in the water cycle
Evaporation and transpiration are lower at night due to lower average temperatures
Downpours in the afternoon because of conventional heating are a feature in global climates can affect infiltration rates
Conventional precipitation is dependant on on direct heating of the ground surface by the sun, often falling in the afternoon when temperatures have reached their maximum - particularly in climatic regions where bulk precipitation is from conventional storms.
Seasonal changes
Controlled by variations of solar radiation
Impacts rates of evapotranspiration and precipitation
Driest parts of lowland England, 80% of precipitation can be lost to evapotranspiration, exhausting the soils river flows are normally at their lowest durning summer
Remote sensing
NOAA polar orbiters - measure cloud liquid water and total precipitable water
ICESAT - measures the surface height of ice sheets