排序方式: 共有27条查询结果,搜索用时 15 毫秒
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Kevin Tansey Jean-Marie GrÉgoire Elisabetta Binaghi Luigi Boschetti Pietro Alessandro Brivio Dmitry Ershov StÉphane Flasse Robert Fraser Dean Graetz Marta Maggi Pascal Peduzzi JOsÉ Pereira JoÃo Silva AdÉlia Sousa Daniela Stroppiana 《Climatic change》2004,67(2-3):345-377
Biomass burning constitutes a major contribution to global emissions of carbon dioxide, carbon monoxide, methane, greenhouse gases and aerosols. Furthermore, biomass burning has an impact on health, transport, the environment and land use. Vegetation fires are certainly not recent phenomena and the impacts are not always negative. However, evidence suggests that fires are becoming more frequent and there is a large increase in the number of fires being set by humans for a variety of reasons. Knowledge of the interactions and feedbacks between biomass burning, climate and carbon cycling is needed to help the prediction of climate change scenarios. To obtain this knowledge, the scientific community requires, in the first instance, information on the spatial and temporal distribution of biomass burning at the global scale. This paper presents an inventory of burned areas at monthly time periods for the year 2000 at a resolution of 1 kilometer (km) and is available to the scientific community at no cost. The burned area products have been derived from a single source of satellite-derived images, the SPOT VEGETATION S1 1 km product, using algorithms developed and calibrated at regional scales by a network of partners. In this paper, estimates of burned area, number of burn scars and average size of the burn scar are described for each month of the year 2000. The information is reported at the country level. This paper makes a significant contribution to understanding the effect of biomass burning on atmospheric chemistry and the storage and cycling of carbon by constraining one of the main parameters used in the calculation of gas emissions. 相似文献
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Modelling storm impacts on beaches, dunes and barrier islands 总被引:10,自引:0,他引:10
Dano Roelvink Ad Reniers Ap van Dongeren Jaap van Thiel de Vries Robert McCall Jamie Lescinski 《Coastal Engineering》2009,56(11-12):1133-1152
A new nearshore numerical model approach to assess the natural coastal response during time-varying storm and hurricane conditions, including dune erosion, overwash and breaching, is validated with a series of analytical, laboratory and field test cases. Innovations include a non-stationary wave driver with directional spreading to account for wave-group generated surf and swash motions and an avalanching mechanism providing a smooth and robust solution for slumping of sand during dune erosion. The model performs well in different situations including dune erosion, overwash and breaching with specific emphasis on swash dynamics, avalanching and 2DH effects; these situations are all modelled using a standard set of parameter settings. The results show the importance of infragravity waves in extending the reach of the resolved processes to the dune front. The simple approach to account for slumping of the dune face by avalanching makes the model easily applicable in two dimensions and applying the same settings good results are obtained both for dune erosion and breaching. 相似文献
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Marc F. P. Bierkens Victoria A. Bell Peter Burek Nathaniel Chaney Laura E. Condon Cédric H. David Ad de Roo Petra Döll Niels Drost James S. Famiglietti Martina Flörke David J. Gochis Paul Houser Rolf Hut Jessica Keune Stefan Kollet Reed M. Maxwell John T. Reager Luis Samaniego Edward Sudicky Edwin H. Sutanudjaja Nick van de Giesen Hessel Winsemius Eric F. Wood 《水文研究》2015,29(2):310-320
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The role of oceanic tide, wind stress, freshwater river inflows, and waves in the long-term circulation and residence time
in óbidos Lagoon is investigated using a sensitivity analysis carried out by means of a two-dimensional model. MOHID modeling
system coupled to Steady-State Spectral Wave model for simulate óbidos Lagoon circulation were implemented. For residence
time calculus, a Lagrangian transport model was used. Tidal forcing is shown to be the dominant forcing, although storm waves
must be considered to simulate accurately the long-term circulation. Tidal forcing enhances a spatial distribution in water
residence time. Renewal time scales varies from values of 2 days in the near-ocean areas and 3 weeks in the inner areas. Freshwater
river inflows decrease the residence time, while waves increase. In heavy rain periods, the water residence time decreases
by about 40% in the upper lagoon. When wave forcing is considered, the residence time increases between 10% and 50% depending
on lagoon area. The increase in residence time is explained by the sea level rise within lagoon (~1 m above average lagoon
sea level) during storm wave periods. Average residence time is 16 days for tidal forcing, 9 days when the rivers are included
(wet period), and 18 days when the waves are considered. 相似文献
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Ad. A. Aliev V. Yu. Lavrushin S. V. Kokh E. V. Sokol O. L. Petrov 《Lithology and Mineral Resources》2017,52(5):358-368
Geochemical studies of pyrite crystals from the mud volcanic ejecta in Azerbaijan were studied. It is shown that all of them have cubic shape. Determination of the sulfur isotope composition revealed a wide variation range of δ34S values from–27.0 to +26.4‰. Signs of spatial zonation were recorded in the distribution of δ34S values—lower values are confined to the present-day coastline of the Caspian Sea. Appearance of pyrite with a high share of 34S is attributed to sulfate reduction that takes place in an environment with excess organic matter. It is supposed that the isotopically heavy sulfides represent the “neck” facies that are formed at the periphery of mud volcanic conduits at the contact of the hydrocarbon-rich mud volcanic fluids with stratal waters of host sediments. 相似文献