Automatic Data Report by the University of British Columbia / Department of Geography
Environmental Prediction in Canadian Cities Measurement Network Vancouver
Database output created on Tue Feb 14 15:51:32 2012
Time period : 01-2008-to-12-2008
Table 1 - Monthly totals of evapotranspiration at 29.00m
| MONTH | Total | Median | Min | Max | No. of Obs. | Percent of data included |
|---|---|---|---|---|---|---|
| (mm/month) | (mm / day) | (mm / day) | (mm / day) | % | ||
| Jan | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Feb | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Mar | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Apr | ------ | ------ | ------ | ------ | 0 | 0.0% |
| May | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Jun | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Jul | 31.95 | 0.93 | ------ | ------ | 1009 | 67.8% |
| Aug | 39.67 | 1.12 | ------ | ------ | 1083 | 72.8% |
| Sep | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Oct | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Nov | ------ | ------ | ------ | ------ | 0 | 0.0% |
| Dec | ------ | ------ | ------ | ------ | 0 | 0.0% |
| TOTAL | ------ | ------ | ------ | ------ | 2092 | 11.9% |
 
Table 2 - Average monthly diurnal course of evapotranspiration at 29.00m (mm / hr)
| HOUR | JAN | FEB | MAR | APR | MAY | JUN | JUL | AUG | SEP | OCT | NOV | DEC |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 00 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0030 | 0.0100 | ------ | ------ | ------ | ------ |
| 01 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0054 | 0.0150 | ------ | ------ | ------ | ------ |
| 02 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0042 | 0.0074 | ------ | ------ | ------ | ------ |
| 03 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0020 | 0.0058 | ------ | ------ | ------ | ------ |
| 04 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0035 | 0.0059 | ------ | ------ | ------ | ------ |
| 05 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0039 | 0.0164 | ------ | ------ | ------ | ------ |
| 06 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0156 | 0.0273 | ------ | ------ | ------ | ------ |
| 07 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0283 | 0.0400 | ------ | ------ | ------ | ------ |
| 08 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0436 | 0.0540 | ------ | ------ | ------ | ------ |
| 09 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0638 | 0.1025 | ------ | ------ | ------ | ------ |
| 10 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0712 | 0.0829 | ------ | ------ | ------ | ------ |
| 11 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0887 | 0.1082 | ------ | ------ | ------ | ------ |
| 12 | ------ | ------ | ------ | ------ | ------ | ------ | 0.1072 | 0.1164 | ------ | ------ | ------ | ------ |
| 13 | ------ | ------ | ------ | ------ | ------ | ------ | 0.1092 | 0.1381 | ------ | ------ | ------ | ------ |
| 14 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0971 | 0.1173 | ------ | ------ | ------ | ------ |
| 15 | ------ | ------ | ------ | ------ | ------ | ------ | 0.1034 | 0.1186 | ------ | ------ | ------ | ------ |
| 16 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0972 | 0.1215 | ------ | ------ | ------ | ------ |
| 17 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0627 | 0.0773 | ------ | ------ | ------ | ------ |
| 18 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0531 | 0.0547 | ------ | ------ | ------ | ------ |
| 19 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0316 | 0.0243 | ------ | ------ | ------ | ------ |
| 20 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0142 | 0.0107 | ------ | ------ | ------ | ------ |
| 21 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0078 | 0.0118 | ------ | ------ | ------ | ------ |
| 22 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0095 | 0.0069 | ------ | ------ | ------ | ------ |
| 23 | ------ | ------ | ------ | ------ | ------ | ------ | 0.0047 | 0.0069 | ------ | ------ | ------ | ------ |