L2 and 3 Flashcards
what are the major components of the water cycle
- precipitation: P, rain or snow
- (evapo)transpiration: ET. evaporation is the conversion of water from liquid to gas from the earth’s surface. transpiration is the evaporation of water through the leaves of plants
- runoff: surface + sub surface runoff. surface runoff is the flow of water that occurs when excess precipitation or meltwater over the land surface flows. subsurface runoff is the waterflow within the saturated soil
- storage: in atmosphere, on surface, and in ground (soil+aquifer)
water balance equation
P = R + ET +- dS
R = P- ET +-dS
what is the global water cycle
water moves from one reservoir to another (atmosphere, ice, fresh/salt water, ground). this circulates naturally and this is the water cycle
water resource availability depends on:
- how much water is in each storage
- when and how fast water moves through the system
- how much water we use
- how clean the water is
what are the main water use sectors
Irrigation/agriculture (70% globally)
domestic water use (11%)
industrial water use (19%)
driving factors behind water use in irrigation
- the size of the area that needs to be irrigated
- crop water requirements (soil moisture high? crop needs less water)
driving factors behind water use in the domestic sector
- size of population
- economic development
- domestic water use intensity
driving factors behind water use in the industry
- economic development
- population density
- manufacturing water use intensity
what are drivers of change in global water resources availability
- socio economic development: population growth so an increase in food/energy/resourcce demands and an increase in sectoral water use. economic development and land use changes
- climate change: the water use for irrigation, domestic use and industry will increase on a global scale
why is there an increasing pressure on our freshwater resources?
- more evaporation due to warmer temperatures, thus the irrigation demand is higher
- excessive water withdrawals in large parts of the world
- groundwater withdrawals –> groundwater depletion happens more in intensively irrigated areas in dryer climates. groundwater depletion is the permanent loss of groundwater from its storage and has more than tripled in the past decade. in the current climate conditions, not all aquifers are recharged
how does CC impact global water availability
mainly by changes in spatial and temporal patterns of precipitation and evaporation.
the longest increase in terrestial precipitation are in the high northern latitude and in the tropics. precipitation and evaporation decreases in S america mediterranean, and S africa. if theres less precipitation there’s also less water available to evaporate. overall decrease in precipitation –> dryer soil. hihger temperature, more evapotranspiration, more runoff, less soil moisture
why use large-scale hydrological models?
- to understand global processes and interactions, e.g. the impacts of CC on water resources availability on a global scale
- to make estimates of water resources availablity now, and in the future. by understanding - current and past trends and anomalies to better predict the future - long term future trends (through scenarios) - forecasting.
overall aim: better water resources management worldwide
what do large-scale hydrological models simulate and what are they used for?
the water cycle and the water balance equation. they are used to
- quantify water resources
- predict floods/droughts
- evaluate cc/land use change impacts
- monitor water quality
VIC WUR model. general characteristics,
vertical infiltration capacity model
- includes the water and energy balance
- accounts for evapotranspiration
-simulates river discharge
- distributed, 50x50 km grid cells
distinguishes 3 soil layers, it accounts for soil moisture content
- human water use is being implemented
VIC WUR model. input and output
input
- hydrological drivers
parametarization
- soil
- land cover/vegetation
- elevation
- flow direction
- reservoirs
- water demands per sector
- aquifer parameters
output:
- river discharge
- soil moisture
- snowmelt
- evapotranspiration
- water uses per sector and return flow
- water table depths, groundwater flow