Objectively Computed Surface Diagnostic Fields PDF Download
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Author: Robert J. Bermowitz
Publisher:
ISBN:
Category : Synoptic meteorology
Languages : en
Pages : 30
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Book Description
Author: Robert J. Bermowitz
Publisher:
ISBN:
Category : Synoptic meteorology
Languages : en
Pages : 30
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Book Description
Author:
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 278
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Book Description
Author:
Publisher:
ISBN:
Category : Aeronautics
Languages : en
Pages : 240
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Book Description
Author: David Harvey Kitzmiller
Publisher:
ISBN:
Category : Severe storms
Languages : en
Pages : 42
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Book Description
Many operational features of the WSR-88D were incorporated specifically to aid forecasters in the detection of severe local storms (damaging winds, large hail, and tornadoes). One interpretive product, the Severe Weather Potential (SWP) algorithm, yields an index proportional to the probability that an individual thunderstorm cell will soon produce any severe weather phenomena. The SWP is based solely on radar information, namely vertically-integrated liquid VIL and storm horizontal extent.
Author: United States. National Weather Service
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 786
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Author: August F. Korte
Publisher:
ISBN:
Category : Meteorology
Languages : en
Pages : 40
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Book Description
The mean maps show average geopotential metric heights for the 850-, 700-, 500-, and 300-mb pressure surfaces at 000 and 1200 GMT for each month of the year. The maps were derived by computer from objectively analyzed grid-point data for November 1961 through January 1969. The use of these maps is briefly described to obtain the average monthly height for any day and 12-hour period
Author: William H. Klein
Publisher:
ISBN:
Category : Precipitation (Meteorology)
Languages : en
Pages : 44
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Author: David Alan Unger
Publisher:
ISBN:
Category : Moisture
Languages : en
Pages : 48
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Book Description
The moisture model used for the Local AFOS MOS Program (LAMP) is described in this paper. The model predicts the degree of saturation in the single layer between 1000 and 500 mb by a moisture parameter known as the saturation deficit. Moisture is advected under the assumption that no evaporation or condensation occurs along the trajectory. The thickness and elevation of the advected air column determine the degree of saturation. Precipitation is forecast when the air column is saturated.
Author: Nancy Westcott
Publisher:
ISBN:
Category : Severe storms
Languages : en
Pages : 128
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Book Description
Author: Ronald M. Reap
Publisher:
ISBN:
Category : Atmospheric temperature
Languages : en
Pages : 32
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Book Description
The Techniques Development Laboratory three-dimensional trajectory model was updated in June 1971 to include the effects of air-sea interactions. Output from the model is currently transmitted via facsimile for use as guidance in severe storm forecasting. Past verification statistics for the model have shown a marked tendency to under-forecast surface temperature and dew point along coastal areas during the cold seasons
