The electrical conductivity of the mantle beneath Europe derived from C-responses from 3 to 720 hr   总被引：6，自引：0，他引：6  

Nils Olsen 《Geophysical Journal International》1998,133(2):298-308

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Causes of low-frequency ground motion amplification in the Salt Lake Basin: the case of the vertically incident P wave     

Kim B. Olsen  Gerard T. Schuster 《Geophysical Journal International》1995,122(3):1045-1061

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Rapid and rhythmic ice sheet fluctuations in western Scandinavia 15-40 Kya–a review     

Lars Olsen  Harald Sveian  Klaas van der  Borg  Bjørn Bergstram  Maarten Broekmans 《Polar research》2002,21(2):235-242

The onshore record of Middle to Late Weichselian sediments and glacial history in Norway indicates a succession of four major ice advances alternating with rapid, considerable ice recessions and interstadial conditions. During all the glacial advances the ice sheet expanded from onshore/inland positions to the shelf areas. The basis for visualizing these variations in glaciation curves constructed along nine transects from inland to shelf, and for interpretation of the palaeoclimatic history, is the regional Quaternary stratigraphy, more than 300 datings, fossil content and some palaeomagnetic data. The methods applied in recent years for AMS radiocarbon dating of glacial sediments with low organic carbon content have given promising results with respect to accuracy and precision, and the results of such datings were an important tool for our reconstructions and for timing of the ice oscillations. The rapid and rhythmic ice fluctuations, as reconstructed in our new model, have been fairly synchronous in most parts of Norway. Ice advances commenced and culminated at 40, 30-28, 24-21 and 18-15 (¹⁴C) Kya. We describe three intervening interstadials from inland sites: Hattfjelldal I, Hattfjelldal II and Trofors. Our stratigraphical record also includes many indications of high, pre-Holocene, relative sea levels, suggesting a considerable glacioisostatic depression of western Scandinavia during the interstadials. In our glaciation model we suggest that, in addition to precipitation, the mountainous fjord and valley topography, glacial isostasy and relative sea level changes were probably more important for the size of the glacial fluctuations than were air temperature changes.  相似文献   

A comparison of biological trends from four marine ecosystems: Synchronies, differences, and commonalities   总被引：1，自引：1，他引：0  

Jason S. Link  William T. Stockhausen  Georg Skaret  William Overholtz  Bernard A. Megrey  Harald Gjster  Sarah Gaichas  Are Dommasnes  Jannike Falk-Petersen  Joseph Kane  Franz J. Mueter  Kevin D. Friedland  Jonathan A. Hare 《Progress in Oceanography》2009,81(1-4):29

Major features of four marine ecosystems were analyzed based on a broad range of fisheries-associated datasets and a suite of oceanographic surveys. The ecosystems analyzed included the Gulf of Maine/Georges Bank in the Northwest Atlantic Ocean, the Norwegian/Barents Seas in the Northeast Atlantic Ocean, and the eastern Bering Sea and the Gulf of Alaska in the Northeast Pacific Ocean. We examined survey trends in major fish abundances, total system fish biomass, and zooplankton biomasses. We standardized each time series and examined trends and anomalies over time, using both time series and cross-correlational statistical methods. We compared dynamics of functionally analogous species from each of these four ecosystems. Major commonalities among ecosystems included a relatively stable amount of total fish biomass and the importance of large calanoid copepods, small pelagic fishes and gadids. Some of the changes in these components were synchronous across ecosystems. Major differences between ecosystems included gradients in the magnitude of total fish biomass, commercial fish biomass, and the timing of major detected events. This work demonstrates the value of comparative analysis across a wide range of marine ecosystems, suggestive of very few but none-the-less detectable common features across all northern hemisphere ocean systems.  相似文献   

VUGS IN ORDINARY CHONDRITES     

Edward Olsen 《Meteoritics & planetary science》1981,16(1):45-59

Large vugs occur in the ordinary chondrite, Farmington. They contain the same phases present in the body of the meteorite, either as vug wall lining or as crystals attached to linings. The morphologies of these phases indicate a history of melting and vapor deposition. These vugs are compared with vugs in the ordinary chondrites, Orvinio and Tadjera, and with published reports of vugs in Rose City and Shaw. It is concluded that although shock events may not cause heating above the liquidus for the body of the meteorite, local pockets of melting and vapor formation do occur due to inhomogenieties in the shock wave pattern. Vugs represent such pockets. Vug formation, as a consequence of shock processing, is widespread among ordinary chondrites and shows no correlation with the average temperature of shock heating, subsequent average cooling rate (as indicated by metallurgical criteria), or blackening of body color.  相似文献   

ELEVEN NEW METEORITES FROM ANTARCTICA, 1976–1977     

Edward J. Olsen  A. Noonan  K. Fredriksson  E. Jarosewich  G. Moreland 《Meteoritics & planetary science》1978,13(2):209-225

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Decadal fingerprints of freshwater discharge around Greenland in a multi-model ensemble   总被引：2，自引：2，他引：0  

Didier Swingedouw  Christian B. Rodehacke  Erik Behrens  Matthew Menary  Steffen M. Olsen  Yongqi Gao  Uwe Mikolajewicz  Juliette Mignot  Arne Biastoch 《Climate Dynamics》2013,41(3-4):695-720

The recent increase in the rate of the Greenland ice sheet melting has raised with urgency the question of the impact of such a melting on the climate. As former model projections, based on a coarse representation of the melting, show very different sensitivity to this melting, it seems necessary to consider a multi-model ensemble to tackle this question. Here we use five coupled climate models and one ocean-only model to evaluate the impact of 0.1 Sv (1 Sv = 10⁶ m³/s) of freshwater equally distributed around the coast of Greenland during the historical era 1965–2004. The ocean-only model helps to discriminate between oceanic and coupled responses. In this idealized framework, we find similar fingerprints in the fourth decade of hosing among the models, with a general weakening of the Atlantic Meridional Overturning Circulation (AMOC). Initially, the additional freshwater spreads along the main currents of the subpolar gyre. Part of the anomaly crosses the Atlantic eastward and enters into the Canary Current constituting a freshwater leakage tapping the subpolar gyre system. As a consequence, we show that the AMOC weakening is smaller if the leakage is larger. We argue that the magnitude of the freshwater leakage is related to the asymmetry between the subpolar-subtropical gyres in the control simulations, which may ultimately be a primary cause for the diversity of AMOC responses to the hosing in the multi-model ensemble. Another important fingerprint concerns a warming in the Nordic Seas in response to the re-emergence of Atlantic subsurface waters capped by the freshwater in the subpolar gyre. This subsurface heat anomaly reaches the Arctic where it emerges and induces a positive upper ocean salinity anomaly by introducing more Atlantic waters. We found similar climatic impacts in all the coupled ocean–atmosphere models with an atmospheric cooling of the North Atlantic except in the region around the Nordic Seas and a slight warming south of the equator in the Atlantic. This meridional gradient of temperature is associated with a southward shift of the tropical rains. The free surface models also show similar sea-level fingerprints notably with a comma-shape of high sea-level rise following the Canary Current.  相似文献   

Upper Devonian tetrapod palaeoecology in the light of new discoveries in East Greenland     

Svend Erik Bendix-Almgreen  Jennifer Alice Clack  Henrik Olsen 《地学学报》1990,2(2):131-137

For the first time, new material of one of the world's oldest known tetrapods, Acanthostega, has been studied in its sedimentological context. The reported evidence suggests that Acanthostega was primarily aquatic and inhabited active fluvial channels in fluvial-dominated environments.  相似文献   

Criticism from former director of fisheries     

A.M. Olsen 《Marine Policy》1982,6(2):140-147

In an article published in Marine Policy a year ago, (Lynne and Brian Chatterton, ‘How much political compromise can fisheries management stand’, Vol 5, No 1, April 1981), it was argued that management of South Australian coastal fisheries reflected the political ideology of the government in power, rather than the biological and socioeconomic imperatives of the resource. In the first article below, A.M. Olsen, former Director of Fisheries, criticizes the Chattertons' conclusions, maintaining that fisheries should be managed by professionals not politicians and that many of Brian Chatterton's problems during his tenure as Minister of Fisheries were of his own making. In the Chattertons' response, they point out that by allocating management of the resource between various vested interests (including government bureaucracy) a minister is making a political decision. In the third article, R.D. Walkerden, a former Permanent Secretary to Fisheries Ministers in South Australia, offers an administrator's view of the controversy. Detailed and parochial as some of the points at issue appear, the debate provides an illuminating view of some of the ideological and organizational conflicts that can hinder the effective management of a coastal resource.  相似文献   

The photometric period of 39 AY Ceti     

J. A. Eaton  D. S. Hall  G. W. Henry  J. L. Hopkins  K. Krisciunas  H. J. Landis  H. Louth  E. H. Olsen  T. R. Renner  H. J. Stelzer 《Astrophysics and Space Science》1983,93(2):271-276

Photoelectric photometry obtained in 1971 and 1972 is compared with that obtained in 1980–81 and 1981–82 to derive a photometric period of 77 ^d .65. JD 2444636.0 is an epoch of minimum light. The full amplitude has been as large as 0 ^m .18 inV. Curiously, the mean light level has dropped by almost 0 ^m .2 over the last ten years. This binary is additionally interesting because of the recently discovered white dwarf secondary component and because unpublished radial velocity measures of Fekel show a large (0.1) eccentricity and an orbital period (57 ^d .1) very different from our photometric period.  相似文献