A. INTRODUCTION
Already examined:
evaporation
moisture transport
condensation & cloud formation
precipitation
What happens to precipitation?
Water budget: local scale examination of the gains, uses, and losses of water
direct precipitation on surface (bare ground), in rivers, lakes, oceans, glaciers
interception by plants
evaporation, overland flow (surface runoff), infiltration

infiltration & percolation
permeability
porosity
zone of aeration
soil water storage
plant uptake & transpiration
evaporation
throughflow
water table
zone of saturation
groundwater flow
aquifer
Gains: precipitation
Soil moisture storage
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Losses: utilization and 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:
evapotranspire (go to the atmosphere)
infiltrate the soil
be used by plants
become groundwater flow
become surface runoff
become stream flow
Water balance - accounting of:
how much water comes in (P)
how much water the atmosphere can take away (PE), and
how much water the atmosphere actually takes away (AE)
Deficits: times of stress for plants and animals
Surplus: times of potential flooding (and stress to humans)