Workshop on Snow Cover and Sea Ice Data

Workshop on Snow Cover and Sea Ice Data
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Publisher :
Total Pages : 132
Release :
ISBN-10 : PSU:000044319328
ISBN-13 :
Rating : 4/5 (28 Downloads)

Synopsis Workshop on Snow Cover and Sea Ice Data by : World Data Center A for Glaciology

U.S. Navy Hindcast Spectral Ocean Wave Model Climatic Atlas

U.S. Navy Hindcast Spectral Ocean Wave Model Climatic Atlas
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Publisher :
Total Pages : 354
Release :
ISBN-10 : UCSD:31822033884214
ISBN-13 :
Rating : 4/5 (14 Downloads)

Synopsis U.S. Navy Hindcast Spectral Ocean Wave Model Climatic Atlas by : United States. Naval Oceanography Command Detachment, Asheville, N.C.

Climatological Marine-fog Frequencies Derived from a Synthesis of the Visibility-weather Group Elements of the Transient-ship Synoptic Reports

Climatological Marine-fog Frequencies Derived from a Synthesis of the Visibility-weather Group Elements of the Transient-ship Synoptic Reports
Author :
Publisher :
Total Pages : 64
Release :
ISBN-10 : UCSD:31822033836222
ISBN-13 :
Rating : 4/5 (22 Downloads)

Synopsis Climatological Marine-fog Frequencies Derived from a Synthesis of the Visibility-weather Group Elements of the Transient-ship Synoptic Reports by : Robert J. Renard

The study presents the essentials of a method of synthesizing the visibility-weather group elements of marine synoptic reports into a computerized scheme for the purpose of deriving frequencies of marine-fog occurrence. The program, based on an interpretation of reporting guidelines in the Synoptic Code Manual, uses 16 combinations of present and past weather, and visibility, to identify fog in the reports. The program then objectively assigns the duration of fog for the period represented by each of the reports. A prototype climatology of marine-fog occurrence for July, over the North Pacific Ocean, is derived from application of the method to a ten-year data base (1963-72). Results are compared and discussed in relation to other published coastal and marine-fog climatologies. Diurnal fog frequencies at sea and the compatibility of fog observations from Ocean Weather Stations and transient ships are also treated. The continuing work and its goals are described.