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An Overview of Climate
Processes The "residence time," or time it takes for a volume of water to cycle-through the system, can vary from a few days in the atmosphere, to a few weeks or months in rivers to 10,000 years or more in icecaps. The time it takes water to cycle through groundwater can vary from weeks and months (shallow aquifers) to hundreds of thousands of years in the case of deep fossil water. Hydrologic variability, particularly
precipitation, is another key component of climate variability, and a
complicated one at that. At a local and regional level, precipitation
can vary widely depending on geography and numerous other factors. Precipitation
also doesn't necessarily correlate with temperature. There can be hot-dry
periods, hot-wet periods, cold-dry periods and cold-wet periods, and everything
in between. See Looking at the Water Budget for
more on hydrologic variability over the course of a year.
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http://www.ncdc.noaa.gov/paleo/ctl/about6.html Downloaded Thursday, 20-Jun-2013 03:10:09 EDT Last Updated Wednesday, 20-Aug-2008 11:22:39 EDT by paleo@noaa.gov Please see the Paleoclimatology Contact Page or the NCDC Contact Page if you have questions or comments. |