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ix TOPIC K - TOPICS UNIQUE TO THE GREENLAND ENVIRONMENT K1 Andersen, A.W., ARCTIC HYDRO-CLIMATIC MEASURE- Thomsen, T. MENTS AND DATABASE - ASSOCIATE TO THE HYDRO-POWER INVESTIGA- TIONS IN GREENLAND K2 Weidick, A. GLACIER INVESTIGATIONS IN CONNECTION WITH FUTURE HYDRO- POWER EXPLOITATION IN GREEN- LAND TOPIC L - MISCELLANEOUS L1 L2 L3 L4 L5 L6 L7 L8 L9 Barstow, S.F., Lygre, A. Bass, D.W., Peters, G.R. Bruun, E., Bruun, P. Bruun, P. Lever, J. H • , Diemand, D. M!kitalo, L.I., Sandkvist, J. Sackinger, W.M. Serson, H.V., Jeffries, M.O., Shoemaker, H.D. Miin-Huey Yan Squire, V.A. Thomsen, A. WAVE MEASUREMENTS IN THE BARENTS SEA: PRACTICAL EXPE RIENCES AND PRELIMINARY RESULTS DYNAMIC ANALYSIS OF UNSTABLE ROLL OF ICEBERGS INDEX FOR PAPERS PRESENTED AT POAC 71, 73, 75, 77, 79, 81, 83, 85 (abstract) ANALOGIES WAVES AND ICE ON SLOPING STRUCTURES MEASUREMENT OF INSTANTANEOUS MOTIONS OF ICE MASSES AT SEA: 1984 PILOT PROGRAM COMBINATION OF WARM WATER OUTLETS AND AIR BUBBLER CUR TAINS FOR ICE-REDUCING PUR POSES - FULL SCALE TESTS ICE ISLAND GENERATION AND TRAJECTORIES NORTH OF ELLES MERE ISLAND, CANADA ON DEFLECTIONS AND STRAINS INDUCED BY LOADS MOVING OVER ICE MAPPING OF SNOWCOVER USING SATELLITE IMAGERY Vol. 2 917 Vol. 2 919 Vol. 2 935 Vol. 2 945 Vol. 2 947 Vol. 2 966 Vol. 2 980 Vol. 2 982 Vol. 2 988 Vol. 2 998 Vol. 2 1009 Vol. 2 1041 Vol. 2 1051
Page 2 and 3: @POAC85 .JAN 8 '86 The 8th internat
Page 4 and 5: TABLE OF CONTENTS (summary): VOLUME
Page 6 and 7: iii A7 Rexford, M.M. INVESTIGATION
Page 8 and 9: C5 Wheeler, J.D., SEA ICE GOUGE STA
Page 10 and 11: vii F15 To, N.M. A METHOD OF CALCUL
Page 14 and 15: PREFACE POAC 85 is the eighth in a
Page 16 and 17: 3 Many Danish authorities, organiza
Page 18: Mr. A. Juliusson University of Icel
Page 21: Mr. A. Weidick The Geologcal Survey
Page 25: Danish Hydraulic Institute Agern Al
Page 28 and 29: 15 LIST OF PARTICIPANTS (June 1985)
Page 30 and 31: 17 Mr. Wang Renshu National Bureau
Page 33: 20 Mr. G.P. Rosendahl Greenland Tec
Page 36 and 37: Mr. E.V. Hansen Municipality of Nuu
Page 39 and 40: SWITZERLAND Mr. L. Rey La Jaquiere
Page 41 and 42: 28 Mr. S.S. Sunder Massachusetts In
Page 44 and 45: W. Dansgaard Geophysical Institute,
Page 46 and 47: 33 Ice divide Fig. 2. Cross section
Page 48 and 49: 35 ...... ·vnIlN''''a DRYAS Dlllin
Page 51 and 52: 3 2550 yr. 2 50% 38 CAMP CENTURY o
Page 53: 40 10. DANSGAARD, W., JOHNSEN, S.J.
Page 60 and 61: 47 indeed very little in common. An
Page 62 and 63:
49 3 ••• SEASONAL DIFFERENTIA
Page 64 and 65:
6 A DELICATE TRADE-OFF: THE CULTURE
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53 *On land, the presence of sensit
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55 communication system of cetacea
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pervasive haze, from December until
Page 72 and 73:
G.E. Frankenstein U.S. Army - CRREL
Page 74 and 75:
Activity Category Seismic explorati
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63 This concern is associated more
Page 78 and 79:
2.4 Plankton 65 Planktonic life, wh
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67 sensitivity to petroleum. Recent
Page 83 and 84:
J. Schwarz Hamburgische Schiffbau
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73 TOPIC A SEA ICE PROPERTIES
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The ice pieces glide along each oth
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81 statistically established distri
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4. RESULTS 84 The results from the
Page 100 and 101:
6. REFERENCES [1] HELLMAN, J-H: "Ba
Page 103 and 104:
Fig. 2. 90 Caisson retained island,
Page 105:
o ! Fig. 4. " /S6 tOOm ! 92 Stress
Page 109:
96 The maximum measured compressive
Page 112 and 113:
ors. During relatively quiet period
Page 117:
104 a. North side of ice island. Sa
Page 123 and 124:
110 fined compression at -2SoC, Kov
Page 125 and 126:
112 Fig. 10. Sidescan sonar record
Page 128 and 129:
115 Ragle, R.H., R.G. Blair and L.E
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118 Fig. 1. Axial double-ball load
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125 (Cox et al., 1984). We tested i
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127 4. Kovacs, A., F. Mlchitti and
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131 The apparatus for testing is ou
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ACKNOWLEDGEMENT 134 The authors wou
Page 149:
FIGURE 2 FIGURE 3. 136 a) b) c) AS
Page 154 and 155:
141 2 NONLINEAR VISCOSITY IN FEM I
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143 the pile are 2.0, 3.0, 5.0, 10.
Page 159:
146 the upper and bottom layer. The
Page 168:
Elev Depth 155 generally determined
Page 184:
4. MICROO"mUCruRAL ANALYSIS 171 FIG
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178 The Fram Strait is the major ic
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180 tions. Structural analysis of t
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186 We found a mixture of inclined
Page 201 and 202:
188 5 RICHTER-MENGE, J.A. & COX, G.
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190 the thermodynamic process will
Page 213:
3.3 Failure mode 200 The ice sheet
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204 promoting the field study and g
Page 219:
206
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209 Sta. Depth (m) Zn (pg/kg) Cd (p
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216 fjord had been flushed in 1982,
Page 233:
Roger Colony Richard E. Moritz Pola
Page 243 and 244:
Jesper Larsen and Asger Kej Danish
Page 247 and 248:
234 the ice compactness A, 0 :iii A
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236 Also for these two levels of mo
Page 251:
REFERNCES 238 1. Wadhams, P., The I
Page 254 and 255:
241 Li FUcheng, Master of Science S
Page 262 and 263:
249 The Choice of Reference Frame f
Page 264 and 265:
251 D , , b , Dc f(z,,')" "if"z",)
Page 267:
254 Table 1. Evaluation of the Solu
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-1300 -1400 -1500 -1600 - 1700 -180
Page 275:
262 of the inclination of the sea s
Page 282:
269 10. PARMETEER, R.R. & COON, M.C
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282 /13/ MATTHEWS, J.B.: Observatio
Page 297:
284 Supply and Services along with
Page 300 and 301:
287 and also on an analog 1/4 inch
Page 302 and 303:
289 gathered only on 17 December 19
Page 308 and 309:
295 2 CRACK I NG AND PACK IIlG OF I
Page 311:
298 takes place. During subsequent
Page 317 and 318:
304 Oa,_ AIr Appr •• t_t.t VI""
Page 319 and 320:
306 Esso's exploratory leases to me
Page 323:
310 Many meteorological and oceanog
Page 329:
316 Ingvar Vik. Senior Research Eng
Page 334:
REFERENCES 321 1 Houmb. O.G. and Vi
Page 348 and 349:
335 vectors, and so will remain nar
Page 351 and 352:
338 7. WADHAMS, P., The effect of a
Page 353 and 354:
340 large ridges in the photo swath
Page 355 and 356:
342 Their routine presence is unamb
Page 357:
344 conditions actually experienced
Page 360:
347 10. Hnatiuk, J., Kovacs, A., Me
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355 structure interaction. It is th
Page 370 and 371:
357 ness in the Sohai Gulf can be c
Page 372 and 373:
3 59 TOPIC C MARINE GEOLOGY AND SOI
Page 377:
364 sity. The mean size has a criti
Page 380 and 381:
367 strong fine-skewed, mesokurtic
Page 382:
REFERENCES 369 1. lowe, J. III, 197
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378 transformed onto the shallow co
Page 396 and 397:
383 changing the data from its true
Page 399 and 400:
REFERENCES 386 1. BARNES, P.W., & R
Page 402:
389 A direct result of the enhanced
Page 406 and 407:
393 W.F. Weeks and W.B. Tucker III
Page 408 and 409:
395 given year sequentially estimat
Page 427 and 428:
414 spatial interval over which sam
Page 432:
C.M.T. WOOdworth-I?iMS Senior Resea
Page 438:
3.3 $1"""""0 T.im1tatioos 425 Scour
Page 443 and 444:
430 Based on the resul ts of the tw
Page 445:
7. REFI!JUH:ES 432 1. Barnes, P., R
Page 450 and 451:
Site 437 'rABLB 1 SIDESCAN IlOSAiC
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440 Figure 3 Location of repetitive
Page 457 and 458:
444
Page 459 and 460:
1. Introduction 446 The composite s
Page 463 and 464:
450 The calculated ultimate load is
Page 468 and 469:
455 A.L. Marshall, Head, Offshore E
Page 470:
maximum at about -70oC. 2.3 Elastic
Page 473 and 474:
460 indicates that moisture content
Page 478 and 479:
465 collision resistance may be inc
Page 480 and 481:
467 2. KIVEKAS, L. et al, Use of co
Page 482 and 483:
469 two-layer system are utilized.
Page 484 and 485:
3 FORMULATION OF THE PROBLEM 471 In
Page 489 and 490:
7 ACKNOWLEDGEMENTS 476 The financia
Page 491 and 492:
478
Page 493 and 494:
480
Page 498 and 499:
485 steel plates in the connections
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487 Unfortunately, what was expecte
Page 503 and 504:
490 Niels Nondal, Civil Engineer, M
Page 505 and 506:
492 vertically in the water (diamet
Page 507 and 508:
494 Spring tide gives high and low
Page 509 and 510:
HW. L.W. __ 496 chored with two (al
Page 512 and 513:
499 could be between the ice barrie
Page 514:
501 In those years tuberculosis was
Page 517 and 518:
504 In addition to quays accommodat
Page 519 and 520:
506 that extensions can take place
Page 521 and 522:
508 the area of the old harbour thr
Page 524:
511 The building of quays at settle
Page 527:
514
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