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PERMAFROST ZONATION AND CLIMATE CHANGE IN THE NORTHERN HEMISPHERE: RESULTS FROM TRANSIENT GENERAL CIRCULATION MODELS 总被引：6，自引：1，他引：5
Numerous studies have demonstrated that both global patterns and local details of permafrost distribution are highly responsive to climatic fluctuations, at several temporal and spatial scales. Permafrost currently underlies about one fourth of the land area of the northern hemisphere, and many qualitative predictions have been made for a severe reduction of this area in response to global warming. A map of permafrost distribution compiled using the frost index, a dimensionless number that can be related to the zonal arrangement of permafrost, shows very good correspondence with a recently published empirical map. The frost index was used in conjunction with three transient general circulation models to compile maps of permafrost zonation for conditions in the mid-21st century. Although regional patterns and local details differ substantially between the three scenarios, all result in reductions in the area occupied by each permafrost zone. Localized expansions of the area underlain by permafrost are apparent from two of the scenarios. Reductions in the areal extent of equilibrium permafrost predicted from two of the three transient models are much less than those indicated by runs using 2 × CO models. 相似文献
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MAXIM G. OGURTSOV OLEG M. RASPOPOV SAMULI HELAMA MARKKU OINONEN MARKUS LINDHOLM HOGNE JUNGNER JOUKO MERILÄINEN 《Geografiska Annaler: Series A, Physical Geography》2008,90(2):141-150
Statistical analysis of a multi-centennial dendrochronological proxy dataset of regional climate, constructed across the latitudinal gradient of 1000 km, was performed. It was shown that centennial ( c. 100 year), tri-decadal (27-32 year), bi-decadal (17-23 year) and decadal (9-13 year) periodicities governed the climate variability in Finland over the last five centuries. Despite the fact that many of the climatic periodicities bore great resemblance to periodicities of solar cycles, little evidence of actual solar influence on Finnish climate was found when the climate proxy records were subjected to linear correlation analysis with sunspot numbers. Highly non-linear response of Northern Fennoscandian climate to solar forcing might be a cause of this result, as well as influence of terrestrial climatic processes (e.g. effect of other forcing factors and internal dynamics of regional climate). Our results show that the presence of internal climate variability at time-scales of solar activity might distort the solar signature in climatic data and complicate its detection. 相似文献
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Glacigenic deposits of the Central Deep: a key to the Late Quaternary evolution of the eastern Barents Sea 总被引：2，自引：0，他引：2
VALERY GATAULLIN LEONID POLYAK OLEG EPSTEIN BORIS ROMANYUK 《Boreas: An International Journal of Quaternary Research》1993,22(1):47-58
Sparker and shallow drilling data indicate that the Quaternary deposits in the Central Deep of the Barents Sea are mainly composed of glacigenic sediments. They comprise basal till and proximal and distal glaciomarine sediments deposited during the last glacial cycle. Apparent glaciotectonic features imply strong glacial erosion of Mesozoic bedrock. The general ice movement is assumed to have been from off Novaya Zemlya and it is concluded that the whole eastern Barents Sea was covered by the Late Weichselian ice-sheet. 相似文献
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OLEG F. VASILIEV 《水文科学杂志》2013,58(2):129-134
Abstract A combined snowfall and snowmelt gauge has been designed and tested to meet the particular conditions commonly found in the British Isles, where snow covers tend to be relatively shallow and short-lived. Current measurement techniques in Britain tend to underestimate both frequency and amount of snowfall. The gauge identifies and measures snow cover by a hydraulic weighing system biased to shallow covers. Snowmelt and rainfall are measured via a central drainage system. Both measurements can be attached to a data logger and could be used in a telemetry network. 相似文献
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MIKHAIL A. GRACHEV SVETLANA S. VOROBYOVA YELENA V. LIKHOSHWAY EVGENY L. GOLDBERG GALINA A. ZIBOROVA OLGA V. LEVINA OLEG M. KHLYSTOV 《Quaternary Science Reviews》1998,17(12):1101-1106
Two parallel drilling cores, BDP96-1 (200 m), and BDP96-2 (100 m), have been taken from top of the underwater Akademichesky Ridge in Lake Baikal and dated by paleomagnetic techniques. These cores are part of the Baikal Drilling Project (Kuzmin et al., 1997a, b). Diatom analysis of the first 100 m of these sediments reveals that they store a 2.5 Myr high-resolution continuous record of the palaeoclimates of East Siberia. Sediments belonging to warmer climates have a high content of diatom algae frustules, whereas those belonging to global glaciations are diatom-barren. The record of Upper Pleistocene (500 kyr BP) strongly correlates with the oceanic SPECMAP curve and contains distinct 100, 41, 23, and 19 kyr periods, as revealed by Fourier analysis. Diversity of diatom species was small in Pliocene. Abrupt and frequent changes of the climate in Pleistocene resulted in frequent dramatic changes in the diatom communities. The extant dominating endemics, Cyclotella minuta and Aulacoseira baicalensis, became important in Lake Baikal 760 kyr and less than 120 kyr BP, respectively. 相似文献
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The Skaergaard intrusion of East Greenland is a gravitationallystratified gabbroic mass that has undergone extreme fractionalcrystallization. Oxygen-isotopic analyses have been obtainedfor the various rock types of this intrusion and for severalcoexisting minerals of these rocks. The general relationshipsamong the O18/O16 ratios of the minerals are the same as havebeen found for other igneous rocks, but the isotopic fracticnationsare smaller, probably as a result of the higher temperatureof formation of the Skaergaard rocks. The later differentiatesare progressively depleted in O18 to a marked degree relativeto the earlier-formed portions of the layered series; the late-stagegranophyres are 4–5 per mil lower in O18/O16 than thelayered Lower Zone gabbros, and are 7–9 per mil lowerthan normal granitic rocks from other localities. This progressivedepletion in O18 is a result of crystallization and settlingout of minerals that are, on the whole, about 1 per mil higherin O18/O16 than the magma liquid. Calculations based on a simplecrystallization model are in agreement with the experimentalresults. 相似文献