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AIDJEX Bulletin #40 - Polar Science Center - University of Washington

AIDJEX Bulletin #40 - Polar Science Center - University of Washington

AIDJEX Bulletin #40 - Polar Science Center - University of Washington

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19. Surface pressure (Val i dated) , <strong>AIDJEX</strong> camps and selected buoys<br />

NavSat systems at the four manned camps and nine NavSat buoys had pressure<br />

sensors to make detailed measurements not specifically included in the surface<br />

pressure charts <strong>of</strong> file 11 above. After appropriate corrections and calibration,<br />

these validated measurements were incorporated into the derivation <strong>of</strong><br />

area-wide geostrophic winds (file 10). These source data are available with<br />

their geographic position at 3-hour intervals. Data are sorted by station.<br />

The manned camps were operational from April 1975 to April 1976. Some <strong>of</strong><br />

the buoys (supplemented by nearby RAMS buoys) continued to operate as late<br />

as 6 December 1976. These data are also incorporated in the alternative<br />

pressure position file noted in data set 9 above.<br />

20. Weather observations , manned camps<br />

Handwritten weather notes logged daily by observers in the manned camps noted<br />

wind velocity, surface pressure, temperature, visibility, and weather. They<br />

back up the digitized data in the files noted above.<br />

21. Logbook entries, manned camps<br />

Members <strong>of</strong> the scientific groups recorded informal notes about events, equipment<br />

performance, changes or calibration <strong>of</strong> sensors, etc. Their logbooks<br />

back up the data collection procedures followed during the main experiment.<br />

22. Wind speed and direction measured by pilot balloon<br />

Pibal measurements using two tarcking theodolites were made each day at the<br />

main camp during the <strong>AIDJEX</strong> experiment. Two generations <strong>of</strong> data are stored<br />

in the data bank. Raw data consist <strong>of</strong> theodolite (angle) measurements taken<br />

at uniform intervals <strong>of</strong> time as the balloon ascended. Drag output (processed<br />

pr<strong>of</strong>iles) give zonal (to the west) and meridional (to the north) velocity<br />

components versus altitude. These data cover the period 10 April 1975 to<br />

20 April 1976 at the main camps.<br />

23. Pr<strong>of</strong>i 1 ing current meter<br />

Twice a day at each manned camp, a current meter was lowered to a depth <strong>of</strong><br />

194 m and raised at a steady rate to determine the stratification <strong>of</strong> the ocean<br />

currents. The analog outputs were digitized to show depth, speed and direction<br />

at uniform depth increments. The data bank has received 300 casts from Caribou,<br />

406 casts from Big Bear, 654 casts from Blue Fox, and 687 casts from Snow Bird--<br />

2047 casts in all to date (10 January 1978).<br />

Note that a cast may either be descending (mode 1) or ascending (mode 2). Each<br />

station usually has two casts, one <strong>of</strong> each mode. Optimally, then, there are<br />

four casts (two stations) per day per camp.<br />

195

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