geog 441 watershed systems precipitation monday 1/26/2009
DESCRIPTION
Precipitation Units- Volume (L 3 ) or Depth/Time (L/T) Input in the mass balance Continuous random variableTRANSCRIPT
GEOG 441Watershed Systems
PrecipitationMonday 1/26/2009
Precipitation
• Characteristics– Spatial– Temporal
• Frequency Analysis
Precipitation
• Units- Volume (L3) or Depth/Time (L/T)• Input in the mass balance• Continuous random variable
Spatial Characteristics
• Point measurements
Spatial Characteristics
• Radar
Spatial Characteristics
• Hyetographs
Temporal Characteristics
• Intensity– Rate of precip over some period of time
• Duration• Frequency
Review
• Histograms• Normal distributions• Extreme value distributions• Cumulative Distributions
• An example with UNC graduate salaries
Review
Normal distributions
meanStd dev
Annual Rainfall
• Assumes data follows normal distribution• Typically works for annual precipitation
data
Annual Precip Trends
0
200
400
600
800
1000
1200
1400
1600
1930 1940 1950 1960 1970 1980 1990 2000
S eattle
S an Diego
Denver
Was hington
Annual Rainfall Histograms and Cumulative Distributions
S eattle His tog ram
02468
1012141618
100300500700900110013001500More
B in
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
F requency
C umulative %
Annual Rainfall Histograms and Cumulative Distributions
S eattle His tog ram
02468
1012141618
100300500700900110013001500More
B in
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
F requency
C umulative %Washington Histogram
0
2
4
6
8
10
12
14
16
18
100 400 700 1000 1300 1600
Bin
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
Frequency
Cumulative %
Annual Rainfall Histograms and Cumulative Distributions
S eattle His tog ram
02468
1012141618
100300500700900110013001500More
B in
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
F requency
C umulative %
Washington Histogram
0
2
4
6
8
10
12
14
16
18
100 400 700 1000 1300 1600
Bin
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
Frequency
Cumulative %
S an Dieg o His tog ram
0
5
10
15
20
25
100 300500 700900110013001500More
B in
Frequency
0.00%
20.00%
40.00%
60.00%
80.00%
100.00%
120.00%
F requenc y
C umulative %
• Different distributions required for shorter time periods
Exceedance Probabilities
• [dimensionless], the relative frequency associated with a random variable attaining a value greater than some specified value.
• For example- calculate probability that annual precipitation in any given year will exceed 1.0 m
Exceedance Probabilities
Exceedance Probability1. Normalize data to a z value
2. Find cumulative probability for a given value (Table A3.2)
Annual Maxima• Takes the highest value for the entire year
Partial Duration
• All values above a certain base• Closely related to annual values for long
return periods• Could be more (frequent) or less
(infrequent) values than annual maxima for a given threshold
Partial Duration Series –RDU Airport
ARI*(years)
1 0.39 1.34 1.56 2.37 2.83 7.92 12.16
2 0.46 1.61 1.86 2.84 3.42 9.32 14.16
5 0.53 1.95 2.29 3.52 4.27 10.83 15.98
10 0.59 2.24 2.65 4.11 4.93 12 17.38
25 0.65 2.58 3.08 4.89 5.83 13.54 19.17
50 0.69 2.83 3.43 5.56 6.54 14.72 20.53
100 0.73 3.08 3.76 6.22 7.26 15.89 21.83
200 0.76 3.31 4.09 6.93 8 17.06 23.09
500 0.79 3.6 4.51 7.88 8.99 18.62 24.7
1000 0.82 3.82 4.84 8.69 9.77 19.8 25.9
60 day
Precipitation Frequency Estimates (inches)
30 day 24 hr 5 min 60 min 120 min 12 hr
Precipitation FrequencyExamples from AZ and NC http://hdsc.nws.noaa.gov/hdsc/pfds/index.html
Return Period
• What is the probability of a storm of X magnitude this year?
• Inverse of exceedance probability
Treturn= (n+1)/mn= # of years of observationm= rank
Return Period- Washington, DCColumn1 Rank Percent Return Per
1433 1 100.00% 511341 2 97.90% 25.51322 3 95.90% 171320 4 93.80% 12.751318 5 91.80% 10.21283 6 89.70% 8.51278 7 87.70% 7.2857141202 8 85.70% 6.3751189 9 83.60% 5.6666671178 10 81.60% 5.1
R eturn P eriod
1
10
100
0 200 400 600 800 1000 1200 1400 1600
S eries 1
Data from Table 2.1 plotted