Assessment of the Impacts of Climate Change on Mountain Hydrology
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Figure A4.12. Correspondence between simulated (continuous thick line) and observed (broken thick line) streamflow at La Balsa gauge station between September 1969 and August 1997
Source: Authors. Note: This is at the lowest pour point before the Cañón del Pato hydroelectric facility, which includes the aggregated response of most glaciated subwatersheds in the Santa River Basin.
Figure A4.13. Mid-monthly calculated and simulated streamflows (m3/s) for three watersheds, 1969–1997 La Balsa—Mid-monthly outflow 1970–1994 (m3/s)
200
Outflow (m3/s)
150
100
50
0
Sep
Oct
Nov
Dec
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Month Total outflow
Glacial outflow
Qobs
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