Definition: The hydrologic cycle describes the continuous movement of water through the atmosphere, hydrosphere, lithosphere, and biosphere.
Components: Involves processes such as evaporation, condensation, precipitation, and runoff.
Key Statistics:
Over 97% of the Earth's water is found in oceans, which dominate evaporation and precipitation globally.
More than 70% of the Earth's surface is covered by oceans.
Water Balance
Evaporation vs. Precipitation:
Over land, precipitation exceeds evaporation + transpiration.
Over water, evaporation exceeds precipitation.
Advection: Each year, land gains 8% more water than oceans lose, which is replenished by runoff.
Moisture Balance of the Atmosphere
Evaporation Sources:
Open water bodies, soil, and plant surfaces contribute to evaporation.
Transpiration: Plants release water that evaporates into the atmosphere, acting as a cooling mechanism.
Actual Evapotranspiration (ACTET):
The actual amount of water that would evaporate/transpire under optimal moisture conditions.
Factors that influence ACTET include energy from the atmosphere, temperature, and solar intensity.
Potential Evapotranspiration (POTET):
Represents the water demand under optimum conditions.
Precipitation
Definition: Precipitation is the primary source of water supply in the hydrologic cycle.
Measurement: Mean Annual Precipitation (1961-1990) is often reported in millimeters, with various ranges indicating levels of rainfall diversity globally.
Water Budget
Components of Water Budget:
Input: Runoff to streams, gravitational water.
Expenditures: Infiltration and percolation.
Computation: The water budget can be analyzed using frameworks like ACTET, POTET, and PRECIP relations, noting conditions for water supply and demand.
Drought
Definition: A drought is a period of below-average precipitation, affecting water supply levels and is defined against climate normals.
Agricultural Drought: Insufficient moisture for crop and pasture growth.
Hydrological Drought: Decrease in water supplies and streamflows.
Socioeconomic Drought: Impacts on economics and community needs.
Groundwater
Importance: Groundwater is a significant source of freshwater, constituting over 22% of global freshwater supplies available for use.
Aquifers: Porous rock layers that store groundwater, replenished slowly over time via surface water.
Types of Groundwater:
Younger and Older Water: Refers to groundwater that has been recharged relatively recently versus that which has been trapped for long periods.
Notable Aquifers:
The Ogallala Aquifer, spanning multiple U.S. states, is a critical water source for agriculture. Water levels in this aquifer exhibit significant declines over recent decades due to extensive use.
Water Use in Texas
Water Source Breakdown (example percentages):
Irrigation: 45.1%
Municipal: 35.3%
Other sectors: 19.6%
Global Water Withdrawal Statistics: Highlighting the diverse withdrawal rates by region indicating potential stress on water resources.
Global Water Stress Projections (2050)
Categories of Stress:
Extremely High (>80%)
High (40-80%)
Medium to High (20-39%)
Low to Medium (10-19%)
Low (
Significance: These projections highlight urgent needs for water management strategies to mitigate water scarcity risks.