Earth's water is distributed across various , with holding the lion's share. Only a tiny fraction is , crucial for human needs. Understanding this distribution is key to managing our limited water resources wisely.
Water balance tracks inputs, outputs, and in a system. This concept is vital for assessing water availability and sustainability at different scales. By analyzing water balance, we can make informed decisions about water management and conservation.
Global Water Distribution and Reservoirs
Global distribution of water resources
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Top images from around the web for Global distribution of water resources
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Earth's water distributed across several reservoirs
Oceans largest reservoir containing ~97% of Earth's water (Pacific, Atlantic, Indian)
and second-largest reservoir storing ~2% of Earth's water (Antarctica, Greenland)
stores ~0.6% of Earth's water
Majority is saline with only a small fraction being fresh water (, )
contains ~0.01% of Earth's water (Amazon River, Great , Lake Baikal)
holds ~0.001% of Earth's water as water vapor (clouds, humidity)
Water moves between these reservoirs through the
Processes include , , , , (water vapor, rainfall, snowmelt)
Freshwater vs saltwater availability
Freshwater resources have low concentrations of dissolved salts (<1,000 mg/L)
Essential for human consumption, agriculture, most industrial processes (drinking water, irrigation, manufacturing)
Limited availability with only ~2.5% of Earth's water being fresh water
Most freshwater locked up in ice caps, glaciers, deep groundwater aquifers (polar regions, mountain ranges)
Surface water and shallow groundwater most accessible freshwater resources (, lakes, )
Saltwater resources have high concentrations of dissolved salts (>1,000 mg/L)
Primarily found in oceans, seas, some inland water bodies (Pacific Ocean, Dead Sea)
Not suitable for direct human use without desalination (reverse osmosis, distillation)
Abundant with ~97.5% of Earth's water being saltwater
Water Balance and Sustainability
Water balance components and scales
Water balance accounts for , outputs, storage changes within a system over time
Based on the principle of : inputs=outputs±changeinstorage
Components of water balance:
: water input from atmospheric moisture (rain, snow, hail)
: water output through evaporation and plant transpiration
: water output as surface flow (streams, rivers)
Groundwater flow (G): water input or output through subsurface flow (aquifers)
: change in water stored within the system (soil moisture, groundwater, surface water)
: P=ET+R+G±ΔS
Spatial scales for water balance analysis:
Local: individual sites or small catchments (farm, forest stand)
Regional: larger watersheds or river basins (Mississippi River Basin, Amazon Basin)
Global: entire Earth's surface
Water balance for sustainability assessment
Water availability compares water inputs with outputs and storage changes
Assessed by comparing precipitation, groundwater recharge with evapotranspiration, runoff ()
occurs when water demands exceed available supplies (droughts, overuse)
balances water use with available supplies for long-term availability and ecosystem health
Requires understanding water balance components and their variability over time
Strategies include:
Improving (drip irrigation, low-flow fixtures)
Enhancing water storage and distribution infrastructure (reservoirs, )
Protecting and restoring natural water sources (, )
Implementing water conservation measures and demand management (, )
Water balance analysis helps identify:
Areas of or deficit (wet vs dry regions)
Seasonal or in water availability (monsoons, El Niño)
Impacts of land use changes, climate change, or other factors on water resources (, )
Opportunities for water resource development or conservation (dams, rainwater harvesting)