首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   411篇
  免费   8篇
  国内免费   5篇
测绘学   11篇
大气科学   24篇
地球物理   92篇
地质学   210篇
海洋学   24篇
天文学   25篇
综合类   4篇
自然地理   34篇
  2022年   3篇
  2020年   5篇
  2019年   6篇
  2018年   9篇
  2017年   8篇
  2016年   14篇
  2015年   8篇
  2014年   14篇
  2013年   20篇
  2012年   17篇
  2011年   18篇
  2010年   19篇
  2009年   36篇
  2008年   18篇
  2007年   15篇
  2006年   16篇
  2005年   17篇
  2004年   8篇
  2003年   9篇
  2002年   8篇
  2001年   9篇
  2000年   5篇
  1999年   5篇
  1998年   6篇
  1997年   5篇
  1996年   4篇
  1995年   4篇
  1993年   4篇
  1992年   4篇
  1989年   3篇
  1986年   3篇
  1985年   4篇
  1984年   5篇
  1982年   4篇
  1979年   3篇
  1975年   3篇
  1971年   5篇
  1970年   3篇
  1969年   3篇
  1967年   3篇
  1966年   3篇
  1962年   3篇
  1959年   3篇
  1954年   3篇
  1953年   2篇
  1952年   2篇
  1939年   2篇
  1938年   3篇
  1937年   2篇
  1936年   2篇
排序方式: 共有424条查询结果,搜索用时 15 毫秒
421.
Phytoplankton biomass is an important factor for short-term forecasts of algal blooms. Our new hydrodynamic-phytoplankton model is primarily intended for simulating the spatial and temporal distribution of phytoplankton in Lake Taihu within a time frame of 1-5 days. The model combines two modules: a simple phytoplankton kinetics module for growth and loss; and a mass-transport module, which defines phytoplankton transport horizontally with a two dimensional hydrodynamic model. To adapt field data for model input and calibration, we introduce two simplifications: (a) exclusion of some processes related to phytoplankton dynamics like nutrient dynamics, sediment resuspension, mineralization and nitrification, and (b) use of monthly measured data of the nutrient state. Chlorophyll-α concentration, representing phytoplankton biomass, is the only state variable in the model. A sensitivity analysis was carried out to identify the most sensitive parameter set in the phytoplankton kinetics module. The model was calibrated with field data collected in 2008 and validated with additional data obtained in 2009. A comparison of simulated and observed chlorophyll-α concentration for 33 grid cells achieved an accuracy of 78.7%. However, mean percent error and mean absolute percent error were 13.4% and 58.2%, respectively, which implies that further improvement is necessary, e.g. by reducing uncertainty of the model input and by an improved parameter calibration.  相似文献   
422.
Abstract

A major goal in hydrological modelling is to identify and quantify different sources of uncertainty in the modelling process. This paper analyses the structural uncertainty in a streamflow modelling system by investigating a set of models with increasing model structure complexity. The models are applied to two basins: Kielstau in Germany and XitaoXi in China. The results show that the model structure is an important factor affecting model performance. For the Kielstau basin, influences from drainage and wetland are critical for the local runoff generation, while for the XitaoXi basin accurate distributions of precipitation and evapotranspiration are two of the determining factors for the success of the river flow simulations. The derived model uncertainty bounds exhibit appropriate coverage of observations. Both case studies indicate that simulation uncertainty for the low-flow period contributes more to the overall uncertainty than that for the peak-flow period, although the main hydrological features in these two basins differ greatly.

Citation Zhang, X. Y., Hörmann, G., Gao, J. F. & Fohrer, N. (2011) Structural uncertainty assessment in a discharge simulation model. Hydrol. Sci. J. 56(5), 854–869.  相似文献   
423.
ABSTRACT

A digital elevation model (DEM), as well as satellite images, was used to detect the changes in the morphology and storage capacity of the Aswan High Dam Reservoir (AHDR) over the past five decades. Study findings indicate that the total storage capacity of the AHDR estimated by the DEM decreased by 12%. This decrease is mainly in the live and the dead storage capacities. The morphology of the reservoir changed in the southern part and at the entrance of the lacustrine part. A gradual conversion of the entrance to the riverine part was observed. The surface area of the AHDR decreased at low water levels because of sedimentation. The average reduction of the surface area between water levels of 140 and 168 m a.s.l. is about 15%, which is equivalent to almost 10 km3.  相似文献   
424.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号