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What happens to precipitation?
Water budget: local scale examination of the gains, uses, and losses of water
Direct precipitation
Interception
throughfall and stemflow
Infiltration
permeability
porosity
Soil water
zone of aeration
soil water storage
plant uptake & transpiration
evaporation
throughflow
percolation
zone of saturation
groundwater flow
aquifer
water table
Overland flow (surface runoff)
Stream flow
Precipitation
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Evapotranspiration
actual evapotranspiration (AE)
potential evapotranspiration (PE)
Simple water balance
moisture abundant environments
P > PE and therefore AE = PE
moisture limited environments
P < PE and therefore AE < PE
seasonal moisture environments
P:
precipitation
DST:
change in storage
PE:
potential evapotranspiration
AE:
actual evapotranspiration
P - PE:
D:
deficit PE - AE
ST:
soil moisture storage (field capacity)
S:
surplus (AE = PE, ST = field capacity, and
excess P is available)
Water Budget for Kingsport, Tennessee
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Year
P
97
99
97
84
104
97
132
112
66
66
66
99
1119
PE
7
8
24
57
97
132
150
133
99
55
12
7
781
P-PE
90
91
73
27
7
-35
-18
-21
-33
11
54
92
XXX
DST
0
0
0
0
0
-35
-18
-21
-26
11
54
35
XXX
ST
100
100
100
100
100
65
47
26
0
11
65
100
XXX
AE
7
8
24
57
97
132
150
133
92
55
12
7
774
D
0
0
0
0
0
0
0
0
7
0
0
0
7
S
90
91
73
27
7
0
0
0
0
0
0
57
345
Water on the earth's surface may:
get evapotranspired (go to the atmosphere)
infiltrate the soil
get used by plants
contribute to groundwater
flow across the surface
end up in rivers & streams
Water balance - accounting of:
how much water comes in (P)
how much water the atmosphere can take away (PE), and
how much water actually goes to the atmosphere (AE)
Deficits: times of stress for plants and animals
Surplus: times of potential flooding (and stress to humans)