Geoscience Reference
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Figure 18.5.
During El Nino phase of the ENSO cycle, warmer-than-usual temperature
regime dominates the Canadian Rocky Mountain regions. The opposite is true during the
La Nina phase, producing above-normal amount of precipitation in the southern regions of
the Canadian Rocky Mountains (Source: National Oceanic and Atmospheric Administration
shtml).
Climate Change Impact in the Canadian Rocky Mountains
A summary of the fi nal agreement which came out of the UN Conference
on Environment and Development (UNCED) that took place in 1992 states,
in part, that:
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