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Hydrology
1.
Hydrology The flow
of water across and through near surface environments
2.
3.
4.
Causes of Precipitation
5.
6.
Biomes and Rainfall
7.
Moisture Sources for
USA
8.
9.
Fig. 4.1 Evaporation
& Transpiration
10.
Fig. 4.4
11.
Plant Transpiration Most
water absorption occurs in upper half of root zone
12.
Annual Pan Evaporation
in USA
13.
Evaporating playa lake
with salts around margin, eastern Washington
14.
15.
16.
17.
Factors Affecting Water
Movement in Soils
18.
19.
20.
21.
22.
23.
24.
Macropore flow, Tennessee
Valley, California
25.
26.
27.
Overland flow, Tennessee
Valley, California
28.
Overland flow, Tennessee
Valley, California
29.
30.
Groundwater & the
Vadose Zone
31.
Groundwater Flow Driven
by hydraulic gradients Q = K I A K is hydraulic conductivity A is cross sectional area I is hydraulic gradient
32.
33.
Hydrographs by Runoff
Mechanism Lag to peak Throughflow SOF HOF Peak Runoff HOF SOF Throughflow
34.
35.
36.
37.
38.
Water balance of
drainage basins Net difference between precipitation and evaporation yields streamflow or groundwater recharge
39.
Gaining and Losing
Streams
40.
Watershed Urbanization
41.
Notas del editor
Figure 2.4-where does the moisture come from Why does ohio get steady rainfall-fronts and convection Compare to other areas in US
The terms in the figure describe the hydrologic character of the basin. Hydrologic data collection best carried out at the basin scale.
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