BIRDS EYE 9-66 21 NOVEMBER-11 DECEMBER.

BIRDS EYE 9-66 observations were scheduled to take advantage of optimum moonlight over the arctic basin. Overall ice concentrations in the arctic basin had reached a maximum of ten-tenths with vast floes being the predominant form and representing an increase in concentration over BIRDS EYE 8-66. Al...

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Bibliographic Details
Main Author: Haggerty, J. J., III
Other Authors: NAVAL OCEANOGRAPHIC OFFICE NSTL STATION MS
Format: Text
Language:English
Published: 1967
Subjects:
Meteorology
Snow
Ice and Permafrost
*ARCTIC REGIONS)
*ARCTIC OCEAN)
(*ICE
(*WEATHER FORECASTING
MARINE METEOROLOGY
SEA ICE
ICE ISLANDS
DISTRIBUTION
SOURCES
COASTAL REGIONS
SEA WATER
POLAR REGIONS
GREENLAND
TERRAIN
CLIMATE
DIURNAL VARIATIONS
ALASKA
AERIAL RECONNAISSANCE
PLAN POSITION INDICATORS
PHOTOGRAPHIC RECORDING SYSTEMS
MOON
ILLUMINATION
BIRDS EYE PROJECT
MOONLIGHT
Arctic
Arctic Ocean
Greenland
Arctic Basin
East Greenland
Ice
permafrost
Sea ice
Alaska
Online Access:http://www.dtic.mil/docs/citations/AD0813397
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0813397
Description
Summary:BIRDS EYE 9-66 observations were scheduled to take advantage of optimum moonlight over the arctic basin. Overall ice concentrations in the arctic basin had reached a maximum of ten-tenths with vast floes being the predominant form and representing an increase in concentration over BIRDS EYE 8-66. Also, considerably more medium floes had been observed during the previous BIRDS EYE. An increase of concentration to ten tenths in Alaskan coastal waters represented an increase of two to three tenths from the previous BIRDS EYE. Normal seasonal increases in ice concentrations occurred along the remaining tracks. Comparison of BIRDS EYE 9-66 data with data for a similar period of 1965 reveals that ice concentrations over the arctic basin were much the same. In east Greenland waters, ice concentrations were two to four tenths lighter than they were during the same period during 1965. The BIRDS EYE 9-66 mission included repeat tracks in the arctic basin after a period of 8 days in order to record short-period changes in ice conditions. Most water opendings were refrozen with very little open water observed on the initial tracks; however, numerous new openings were observed on repeated tracks during and after the passage of a well-developed low-pressure system. Many new topographic features were noted. Flying conditions were generally poor. Clouds obscuring the moon hampered water opening and ridge counts. (Author)

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