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V. I. Bychkova M. M. Kurbatova G. A. Zarochentsev R. Yu. Ignatov 《Russian Meteorology and Hydrology》2018,43(7):444-448
The object under study is the blowing snow, i.e., the transport of snow lifted from the snow surface. The method is described for predicting the blowing snow initiation using the output data of the WRF-ARW numerical atmospheric model. The skill scores are presented for the forecasts for January 2013 calculated from data of 10 stations of the Canadian weather observation network. 相似文献
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O. A. Deshcherevskaya V. K. Avilov Ba Duy Dinh Cong Huan Tran J. A. Kurbatova 《Izvestiya Atmospheric and Oceanic Physics》2013,49(8):819-838
A method of using the standard network weather station data for local ecosystem research is considered on the example of the modern climate of the Cát Tiên National Park (Southern Vietnam) and local climate change in 1980–2010. Special attention is focused on the environmental parameters, which play a role of the limiting factors. It is shown that the climate of Southern Vietnam responds with statistical significance to global climate change. Suggestions about the possible reactions of tropical monsoon forest ecosystem to climate change are given. 相似文献
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V. N. Sinyukovich N. N. Kurbatova I. A. Chernyavskaya 《Geography and Natural Resources》2011,32(1):54-59
Based on experimental data on the level and elements of the water balance of the Ust’-Ilimsk reservoir, we outline the characteristic
properties of the long-term and seasonal regimes of its impounding and drawdown under normal operation conditions (1977–2008).
We demonstrate the role played by the individual components of water input and output in the formation of the reservoir’s
water regime. 相似文献
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A final paper on water-level monitoring from space outlines principles for the use of space imagery in interpretation of short-term changes in the position of shorelines and coastal water levels resulting from storm surges and strong offshore winds. Over 100 images of various types, seasons, and storm-surge conditions, carefully referenced with field data on slope, vegetation cover, water level, and wind direction, were used to determine “maximal” and “minimal” positions of the Caspian shoreline for the period 1973-1983. This information is useful in understanding the seasonal regime of water-level fluctuations and anticipating flooding associated with winds of a given velocity. Translated from: Izvestlya vysshikh uchebnykh zavedenly, geodeziya i aerofotos'yemka, 1986, No. 4, pp. 93-97. 相似文献
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V. N. Sinyukovich L. N. Sizova M. N. Shimaraev N. N. Kurbatova 《Geography and Natural Resources》2013,34(4):350-355
We examine the changes in water inflow into Baikal that are taking place due to global warming that enhanced beginning in the 1970s as well as due to the different responses of discharges of separate rivers within the Baikal watershed basin to climate change. 相似文献
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Yushkov V. P. Kurbatova M. M. Varentsov M. I. Lezina E. A. Kurbatov G. A. Miller E. A. Repina I. A. Artamonov A. Yu. Kallistratova M. A. 《Izvestiya Atmospheric and Oceanic Physics》2019,55(5):389-406
Izvestiya, Atmospheric and Oceanic Physics - Using the example of an analysis of an extreme lowering of temperature in Moscow in January 2017, the horizontal and vertical extent of the urban heat... 相似文献
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E. P. Dubinin A. V. Kokhan D. E. Teterin A. L. Grokhol’sky E. S. Kurbatova N. M. Sushchevskaya 《Geotectonics》2016,50(1):35-53
Western, central, and eastern provinces are recognized in the Scotia Sea. They are distinguished by their bottom topography, geophysical characteristics, and crustal structure, which record their different origin and evolution. The western province is characterized by the oceanic crust that formed on the West Scotia Ridge, where active spreading may have ceased as a result of a collision between propagating rift and the structural barrier of the thick continental lithosphere of the Falkland Plateau. The central province is a series of blocks mainly composed of continental crust that subsided to various depths depending on the degree of extension in the course of rifting. These blocks are separated by local areas with oceanic crust formed due to the breakup of the continental crust and diffusive spreading. These areas are characterized by deep bottom and high values of Bouguer anomalies. The southern framework of the central province consists of subsided continental blocks and microcontinents divided by small spreading-type basins formed by lithospheric extension complicated by strike-slip faulting. The eastern province is composed of oceanic crust formed on the backarc spreading East Scotia Ridge. The results of density analysis, analog, and numerical simulations allowed us to explain some features of the structure and evolution of these provinces. The insight into tectonic structure of the provinces and their evolution allowed us to recognize several types of riftogenic basins differing in geodynamics, age, and geological and geophysical characteristics. 相似文献
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