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Hydrology The flow of water across and through near surface environments
 
Precipitation ,[object Object],[object Object],[object Object]
Causes of Precipitation
[object Object],[object Object],[object Object],Weather vs. Climate Patterns
Biomes and Rainfall
Moisture Sources for USA
 
Fig. 4.1 Evaporation & Transpiration
Fig. 4.4
Plant Transpiration Most water absorption occurs in upper half of root zone
Annual Pan Evaporation in USA
Evaporating playa lake with salts around margin, eastern Washington
 
 
Water Flow Hillslope Hydrology ,[object Object],[object Object],[object Object],[object Object],[object Object]
Factors Affecting Water Movement in Soils
[object Object],[object Object],[object Object],[object Object],[object Object],Runoff Generation
[object Object],Horton Overland Flow
 
[object Object],[object Object],[object Object],Horton Overland Flow
[object Object],[object Object],[object Object],[object Object],Horton Overland Flow
Subsurface Stormflow ,[object Object],[object Object]
Macropore flow, Tennessee Valley, California
Saturation Overland Flow ,[object Object],[object Object]
 
Overland flow, Tennessee Valley, California
Overland flow, Tennessee Valley, California
[object Object],Direct Precipitation on Channels
Groundwater & the Vadose Zone
Groundwater Flow Driven by hydraulic gradients Q = K I A K is hydraulic conductivity A is cross sectional area I is hydraulic gradient
 
Hydrographs by Runoff Mechanism Lag to peak Throughflow  SOF HOF Peak Runoff HOF SOF Throughflow
 
 
 
 
Water balance of drainage basins Net difference between precipitation and evaporation yields streamflow or groundwater recharge
Gaining and Losing Streams
Watershed Urbanization
 

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Hydrology

Hinweis der Redaktion

  1. Figure 2.4-where does the moisture come from Why does ohio get steady rainfall-fronts and convection Compare to other areas in US
  2. The terms in the figure describe the hydrologic character of the basin. Hydrologic data collection best carried out at the basin scale.