Prognosis of the 700-mb Temperature Field and the 1000-500-mb Precipitable Water Field.
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Prognosis of the 700-mb Temperature Field and the 1000-500-mb Precipitable Water Field. by Canada. Dept. of Transport. Meteorological Branch.

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Published by s.n in S.l .
Written in English


Book details:

Edition Notes

1

ContributionsHarley, W.S.
ID Numbers
Open LibraryOL21868517M

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ture at a given level because it represents a vertical mean of temperature. In winter precipitation situations, the temperature rarely is warmer than zero degrees Celsius at altitudes ab feet, Thus the thick- ness between the mb and mb levels is theoretically the best para- Size: 1MB. Surface, mb, mb Winds and Equivalent Potential Temperature, mb, mb Winds and Temperature, mb, mb Corpus Christi Sounding Radar Loops: One and Two. NOTES: (1) The to mb Thickness provides clues as to whether there is warm air aloft. (2) If complete melting of precipitation occurs ( - mb thickness greater than 1, gpm), precipitation will fall as rain if surface temperature is above freezing or freezing rain if the surface is freezing. Surface temperature is the discriminator of rain versus freezing rain (0 C threshold). The mb CMC anysis for 12Z 10 Oct shows contours of mb height and mb thickness. Equivalent barotropic systems (black circles) can be seen over the Pacific Ocean, where the jet stream flows paralell to the thickness gradient, and in "cutoff lows" in the arctic, which correspond to regions of isolated cold pools.

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