Large asymmetrical temperature trends at Mount Wilson, California

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Atmospheric Composition And Structure: Pollution-Urban And Regional, Meteorology And Atmospheric Dynamics: Boundary Layer Processes, Meteorology And Atmospheric Dynamics: Climatology, Meteorology And Atmospheric Dynamics: Land/Atmosphere Interactions

Scientific paper

We compiled and analyzed a daily time series of temperatures and precipitation totals from Mount Wilson, California from 1918 to 1998. Our results show a large decline in maximum temperature, no change or an upward trend in minimum temperature, and a substantial decline in the diurnal temperature range (DTR). The interannual variations in monthly maximum temperature and DTR are significantly correlated with monthly precipitation levels, sea-surface temperatures (SSTs) off the coast of Southern California, and the Southern Oscillation Index (SOI). El Niño periods and/or months with high SST anomalies tend to be wet with lower maximum temperatures and DTR while La Niña periods and/or months of lower SSTs are hotter and drier with higher DTR values. It is noteworthy that the SOI and SSTs have significant trends toward more El Niño-like conditions with higher SSTs off Southern California.

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