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1. |
Background to Otto Sverdrup's voyage in the Kara Sea on boardeclipsein 1914–1915 |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 167-171
William Barr,
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ISSN:0273-8457
DOI:10.1080/10889379109377458
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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2. |
The expedition on boardeclipsein search of the expeditions of lieutenant Brusilov and the geologist rusanov (Preliminary report) |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 172-202
I. Trzhemesskiy,
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ISSN:0273-8457
DOI:10.1080/10889379109377459
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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3. |
The reaction of glaciers to impending climatic change |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 203-217
V. M. Kotlyakov,
M. G. Grosswald,
M. B. Dyurgerov,
V. L. Mazo,
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摘要:
The focus of the article is the negative changes which can be expected in the world's glaciers associated with possible “greenhouse”; warming of the climate. It examines the mechanisms of the instability of marine ice sheets, which may lead to their catastrophic collapse and to a rise in sea level of 5–7 m over the next few decades. Calculations have been made concerning the extreme regimes of mountain glaciers in temperate and subtropical latitudes, which would involve a sharply negative mass balance (up to ‐3 to ‐5 m per year); this regime will lead to a rapid disappearance of these glaciers.
ISSN:0273-8457
DOI:10.1080/10889379109377460
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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4. |
Primary productivity of the tundra and polar deserts of the USSR |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 218-227
G. Ye. Vil'chek,
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摘要:
An analysis of primary productivity reveals a valid positive correlation with climatic indices (mean July temperature, degree days above 0°C, and summer precipitation) when one compares polar deserts, arctic tundra and typical subarctic tundra. This correlation does not apply, however, when one compares typical and southern subarctic tundra. The analysis also suggests that there are viable grounds for distinguishing polar deserts, arctic tundra, and subarctic tundra as independent zones, rather than classing the arctic tundra and subarctic tundra as subzones of the tundra zone.
ISSN:0273-8457
DOI:10.1080/10889379109377461
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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5. |
Use of the ecologo‐geographical method in palynological investigations of theyedomaformations of northeastern USSR |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 228-234
A. N. Simakova,
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摘要:
Spore‐ and pollen diagrams from samples at five different depths in theyedomasediments of the Duvanyy Yar exposure on the Kolyma River were analyzed. For each sample range diagrams (diagrams of percentage occurrence of the species identified in the sample, in terms of the present vegetation) were compiled in order to locate the best match in terms of species composition in the present vegetation. This technique permits an evaluation of the probable climate at the time of deposition. The results indicate that the oldest deposits (at a depth of 47 m) correlate with the second period of the Zyryan Glaciation; samples at higher levels derive from the Kargin Interstadial and the subsequent Sartan glacial phase. The range diagram technique suggests that conditions during the Kargin Interstadial matched those of the Holocene quite closely.
ISSN:0273-8457
DOI:10.1080/10889379109377462
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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6. |
The structure and origin of the East Novaya Zemlya trough |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page 235-242
N. N. Dunayev,
O. V. Levchenko,
L. R. Merklin,
Yu. A. Pavlidis,
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摘要:
The authors present a description of the structure and morphology of the East Novaya Zemlya Trough, running parallel to the axis of Novaya Zemlya in the western part of the Kara Sea. Having analyzed the available data on the structure of the trough and the unconsolidated sediments within it, they conclude that the tectonic movements responsible for its origin began at the Paleogene/Neogene boundary. While some relatively minor movements occurred at the late Pleistocene/Holocene boundary, these simply represented the latest in a long series of such movements and were not responsible for the major features of the trough, as some authors have suggested. Although some glacial scouring of the trough has occurred, glacial erosion is not primarily responsible for its present form, nor is glacio‐isostatic depression responsible for any significant proportion of its depth.
ISSN:0273-8457
DOI:10.1080/10889379109377463
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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7. |
Editorial board |
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Polar Geography and Geology,
Volume 15,
Issue 3,
1991,
Page -
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PDF (66KB)
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ISSN:0273-8457
DOI:10.1080/10889379109377457
出版商:Taylor & Francis Group
年代:1991
数据来源: Taylor
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