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

More documents

Recommendations

Info

TABLE 1 STRETCHING, STRESS, ASP CHARACTERISTIC DIRECTION PARAMETERS FOR SIMPLE HOMOGENEOUS FIELDS -1 0 -112 -112 0 n -1.00 -1.00 n/2 none Sa -&I2 &I2 0 4 1 2 0 3n/4 -0.67 -1.11 nI4 0 5b -112 h/2 $-l+ 5) $-1-m 0 2n/3 -0.55 -1.10 n/6 t27.4 5c 0, 1 112 -112 0 nI2 -0.26 -0.93 0 f45.0 5d 112 hl2 +A) +cl-A, 0 n/3 0.00 -0.44 -n/6 262.6 5e m 2 &I2 JT/2 0 0 714 0.04 -0.20 -n14 90 5f 132
- W L - I- 0 a e I- Z 0 u u -' a 0 a I- O v, - 1 1 1 1 1 A 0 Y 133
Page 2 and 3:
DATA BUOYS AIDJEX BULLETIN No. 40 J
Page 4 and 5:
NOTE TO FRIENDS, AND BYSTANDERS . .
Page 6 and 7:
SUMMARY OF TECHNICAL DEVELOPMENTS I
Page 8 and 9:
milestones, kept the vendor working
Page 10 and 11:
The scene during deployment of HF-N
Page 12 and 13:
The initial AIDJEX scientific plan
Page 14 and 15:
poizr-orbiting satellite, which is
Page 16 and 17:
t@ the spacecraft during each orbit
Page 18 and 19:
BUOY NAHE COMMUN. COMMANDS FIXES TA
Page 20 and 21:
L( 0 I 2 3 4 3 Radial error, kilome
Page 22 and 23:
The buoy will be subjected to tempe
Page 24 and 25:
nics occupy about 12 feet of the 17
Page 26 and 27:
Ill -- - KEY AIUJEX WIN WW AEBa 0 4
Page 28 and 29:
event that a melt pond should form
Page 30 and 31:
chute supplied by Paranetics Inc. i
Page 32 and 33:
6'" IqORGANIC LITHIUM BP.TTEI?Y IMP
Page 34 and 35:
OM (AD RAMS) UREMEN~ \ AIRDROP N m
Page 36 and 37:
provides a grid from which geostrop
Page 38 and 39:
words; a four-bit air temperature w
Page 40 and 41:
PERFORMANCE OF MET/OCEAN BUOYS IN A
Page 42 and 43:
Sensor samples were taken every thr
Page 44 and 45:
strengths are known, were used with
Page 46 and 47:
the ice (causing reduced shear). An
Page 48 and 49:
(McPhee, Mangum, and Martin) , TABL
Page 50 and 51:
70°N 75'N n 3 P 17OOW (D Y 170°W
Page 52 and 53:
12OOW * U Station 25. Xeasurements
Page 54 and 55:
(McPhee , Mangum, and Martin) 2701
Page 56 and 57:
(McPhee, Mangum, and Martin) a 0 a
Page 58 and 59:
"i BUOY 4 I 43 360- 309- 257 206 15
Page 60 and 61:
a30gl 251 I 60 511 r 43 BUOY 4 I
Page 62 and 63:
n 4, (McPhee, Mangum, and Martin) 8
Page 64 and 65:
(McPhee, Mangum, and Martin) 33 W c
Page 66 and 67:
. '-,..I.. . B A R R O W W I N D S
Page 68 and 69:
:
Page 70 and 71:
I 25 23 t h--:!li[ NCI PiHCEl4l 22
Page 72 and 73:
.5 .4 .3 0 A R 2 R 0 W J - 0 B U -
Page 74 and 75:
9 1.5 1.0 c 8 w .5 R 930 $ 565 1000
Page 76 and 77:
Clock corrections were applied rout
Page 78 and 79:
Q) u o z z i 4- 4- Z + + z f n 9 Ef
Page 80 and 81:
TABLE 1 DIFFERENCES IN DAILY TEMPER
Page 82 and 83:
Laboratory calibration of the ADRAM
Page 84 and 85: 3.20- - 1 t W o? 2 3.051 ...:-.;..
Page 86 and 87: POSITION MEASUREMENTS OF AIDJEX MAN
Page 88 and 89: some redundancy. Four points were u
Page 90 and 91: 75.5 75.: - E75.1 LLI % y75.c - 1 1
Page 92 and 93: The translocation principle removes
Page 94 and 95: POSITION ACCURACY To evaluate the q
Page 96 and 97: TABLE 1 STAND-ALONE ACCURACY 68th P
Page 98 and 99: Az i mu t h s When both receivers a
Page 100 and 101: DATA PROCESSING Following the field
Page 102 and 103: model ice motion in the statistical
Page 104 and 105: FREC 1 INCY / DOPPLER / FREQUENCY /
Page 106 and 107: 35 30 25 v) > 0 2 20 LL 0 r= E m 15
Page 108 and 109: An example of a large-scale buoy ar
Page 110 and 111: observations are needed in remote a
Page 112 and 113: useful for determining how various
Page 114 and 115: as well as velocity fields, we must
Page 116 and 117: Since small changes in the yield su
Page 118 and 119: The transformation of the system of
Page 120 and 121: e able to judge how well such a mod
Page 122 and 123: then the flow rule becomes Q = +A -
Page 124 and 125: [-B' -F Finally, we eliminate Carte
Page 126 and 127: differential equation. 2. Discontin
Page 128 and 129: Substituting (36) and (37) into (34
Page 130 and 131: arbitrarily assign the values of 1
Page 132 and 133: The special case when advection can
Page 136 and 137: ate of deformation, we have normali
Page 138 and 139: CHARACTERISTIC EQUATIONS The ordina
Page 140 and 141: One way to circumvent the problems
Page 142 and 143: The equations governing solutions a
Page 144 and 145: It is readily seen that when body f
Page 146 and 147: which may be substituted into equat
Page 148 and 149: a the stress derivative dCldS remai
Page 150 and 151: Although we have not studied in thi
Page 152 and 153: Courant, R., and D. Hilbert. 1962.
Page 154 and 155: A RESEARCH PLAN TO TEST THE AIDJEX
Page 156 and 157: the barges managed to reach their d
Page 158 and 159: APPROACH A baseline simulation 0-f
Page 160 and 161: SENSITIVITY OF ICE RESPONSE TO DIFF
Page 162 and 163: Since free drift of ice is computed
Page 164 and 165: and what is observed becomes less i
Page 166 and 167: stresses appear to be relatively un
Page 168 and 169: ehavior is directly related to accu
Page 170 and 171: TABLE 1 COMPARISON OF ESTIMATED ERR
Page 172 and 173: a) Base line b) 24-hour prediction
Page 174 and 175: \ / a) Base line b) 24- hour predi
Page 176 and 177: a) Base line b) 24- hour predi ct i
Page 178 and 179: a) Base line b) 24-hour prediction
Page 180 and 181: \ / a) Base line b) 24-hour predict
Page 182 and 183: .. a) Base line b) 24- hour predict
Page 184 and 185:
J2 a) Base line b) 24-hour predicti
Page 186 and 187:
) 24-hour prediction c) 36-hour pre
Page 188 and 189:
a) Base line b) 24-hour prediction
Page 190 and 191:
8 Figure 17. AIDJEX surface pressur
Page 192 and 193:
APPENDIX 1 AIDJEX DATA FILES 1. Pos
Page 194 and 195:
9A. Surface-1 eve1 ai r pressure (d
Page 196 and 197:
19. Surface pressure (Val i dated)
Page 198 and 199:
APPENDIX 2 AIDJEX DATA TRANSFERRED
Page 200 and 201:
I -7-71327GEO A Cards (continued) 7
Page 202:
B Cards (continued) 201
show all

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

Create successful ePaper yourself

Delete template?

Save as template?