This week is Spring vacation week for DataStreme Atmosphere. This DataStreme Atmosphere Daily Summary contains Historical Weather Events for this date. In addition, new items appear in the Weekly Weather and Climate News. The Investigation and Supplemental Information…In Greater Depth files from last week will remain on the DataStreme Atmosphere Homepage and the Concepts of the Day for Tuesday and Thursday will be repeated for those who may have been on spring break. If you have questions, check with your mentor. Current weather data are available on the homepage as usual. Current weather data are available on the homepage as usual. If you are looking for an alternative description of daily weather, you could try:
http://www.usatoday.com/weather/default.htm
(USA Today)
or
http://www.weather.com/newscenter/nationalforecast/index.html
(The Weather Channel)
The usual DataStreme Atmosphere Daily Summaries and Investigation files will return next week, beginning on Monday, 22 March 2010.
Note: This Concept and accompanying questions represent a repeat of the Concepts and questions that were posted last Tuesday, 9 March 2010.
The chemical compound that we call water is a unique substance in that it can exist in three phases within the ranges of temperatures and pressures found in the atmosphere. At very cold temperatures, water is a solid, ice, which covers our lakes and puddles. Warm it some and it melts to liquid that covers almost two-thirds of the Earth and falls from clouds above. At all typical temperatures, some water exists in the invisible vapor phase. The transition between these forms is crucial to the conditions we associate with "weather". A volume, even without air in it, has a maximum capacity for vapor that depends on the temperature. As the temperature rises, more ice can sublimate or water can evaporate to provide additional vapor for the volume. As the temperature falls, some vapor must condense back to the liquid or solid form. The maximum amount of vapor in the volume at its associated temperature produces the condition called saturation.
Normally a volume of air is not saturated, meaning that less than the maximum possible vapor is present. Saturation can occur in one of two ways. More vapor can be added to the volume to reach the maximum. This addition is seen just above the spout of a boiling teakettle, or with so-called steam fog, a version of your breath on a cold day. Generally the atmosphere creates saturation a second way, by cooling the air volume to reach saturation with the amount of vapor originally present. Cooling to saturation can be by one of two processes. Rising air cools as it expands into lower surrounding pressures at higher altitudes. Saturation and clouds can result. Overnight radiational cooling near the ground may create fog.
For more information describing the global hydrological cycle, you may consult the optional material in Tuesday's Supplemental Information…In Greater Depth.
To be submitted on the lines for Tuesday on the Investigations Manual, Week 6 Chapter Progress Response Form, under section B. Daily Summary.
From the files of the Aviation Weather Center, Kansas City, MO and Intellicast
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Prepared by Edward J. Hopkins, Ph.D., email hopkins@meteor.wisc.edu
© Copyright, 2010, The American Meteorological Society.