ESS Topic 4.1
Hydrological Cycle Overview
The movement of water is termed stream flow.
Water cycles through streams, rivers, lakes, and ultimately to the seas, some eventually evaporating into the atmosphere.
Processes of Water Flow
During heavy rainfall or rapid snow/ice melt, rivers and lakes can overflow, causing flooding, which damages both ecosystems and human settlements.
Abstracting Water: Humans extract water from rivers and lakes, termed abstraction.
Water Transformation Processes
Water changes state through various processes in the water cycle:
Evaporation: Liquid to gas.
Condensation: Gas back to liquid.
Freezing: Liquid to solid.
Melting: Solid to liquid.
The Continuous Water Cycle
All water on Earth is ancient; it is a continuous loop of precipitation, evaporation, and movement.
Life on Earth relies on a functioning water cycle: "flows and stores" embody the system of water movement between storage areas like oceans, glaciers, lakes, rivers, and underground aquifers.
Types of Precipitation
Precipitation includes rain, snow, hail, sleet, fog, and mist, falling onto various surfaces (oceans, rivers, land).
Interception occurs when vegetation captures precipitation before it hits the ground.
Groundwater is formed through infiltration and percolation into different soil layers.
Movement of Groundwater
Groundwater flows laterally towards bodies of water.
Deeper flows tend to be slower, ranging from years to millions to resurface.
Evaporation and Transpiration
Evaporation returns water to the atmosphere, driven by solar heat.
Transpiration: Plants release water vapor through their leaves; combined with evaporation from other sources is termed evapotranspiration.
Ocean Circulation and Currents
Ocean currents are influenced by temperature, salinity, wind, tides, and Earth's rotation (Coriolis effect).
Two Types of Currents:
Surface Currents: Affect the upper 10% of ocean water.
Deep Ocean Currents: Affect 90% of ocean water; driven by density differences in seawater.
Global Conveyor Belt
A system created by thermal haline circulation and surface currents, distributing nutrients and water globally but moving slowly (1 cm per second).
Potential impact of global warming includes slowing currents, which can disrupt weather patterns.
Human Impact on the Hydrological Cycle
Factors such as irrigation, industrialization, and population growth put pressure on freshwater supplies.
Global warming can alter rainfall patterns, impacting water availability.
Future Learning
Next class will focus on water testing and access to clean drinking water
Key Vocabulary for Hydrological Cycle:
Precipitation, runoff, interception, infiltration, percolation, discharge, transpiration, evaporation, condensation.