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941.
Mechanisms for the spatio-temporal development of the Tropical Pacific Meridional Mode(TPMM) are investigated using a coupled ocean-atmosphere model and observations.In both observations and the model,this meridional mode displays decadal variations and is most pronounced in spring and early summer.The model simulation suggests that once SST anomalies in the subtropical northeastern Pacific are initiated,say by northeasterly trade wind variability,perturbations evolve into a merdional dipole in 2-3 months.A... 相似文献
942.
Simulations of the Tropical Intraseasonal Oscillation by the Atmospheric General Circulation Model of the Beijing Climate Center 总被引:1,自引:0,他引:1 下载免费PDF全文
The performance of BCC (Beijing Climate Center) AGCM 2.0.1 (Atmospheric General Circulation Model version 2.0.1) in simulating the tropical intraseasonal oscillation (TIO) is examined in this paper.The simulations are validated against observation and compared with the NCAR CAM3 (Community Atmosphere Model version 3) results.The BCC AGCM2.0.1 is developed based on the original BCC AGCM (version 1) and NCAR CAM3.New reference atmosphere and reference pressure are introduced into the model.Therefore,the origi... 相似文献
943.
Assessing the Influence of the ENSO on Tropical Cyclone Prevailing Tracks in the Western North Pacific 总被引:3,自引:0,他引:3
Using a statistical model for simulating tropical cyclone (TC) formation and a trajectory model for simulating TC tracks, the influence of the El Nino-Southern Oscillation (ENSO) on the peak-season (July-September) TC prevailing tracks in the western North Pacific basin is assessed based on 14 selected El Nino and 14 selected La Nina years during the period 1950-2007. It is found that the combination of statistical formation model and a trajectory model can simulate well the primary features of TC prevai... 相似文献
944.
In this paper, the role of westerly winds at southern high latitudes in global climate is investigated in a fully coupled ocean-atmosphere general circulation model. In the model, the wind stress south of 40°S is turned off with ocean and atmosphere fully coupled both locally and elsewhere. The coupled model explicitly demonstrates that a shutdown of southern high latitude wind stress induces a general cooling over the Antarctic Circumpolar Current (ACC) region, with surface Ekman flow and vertical mixing p... 相似文献
945.
Direct Climatic Effect of Dust Aerosol in the NCAR Community Atmosphere Model Version 3 (CAM3) 总被引:3,自引:0,他引:3
Direct climate responses to dust shortwave and longwave radiative forcing (RF) are studied using the NCAR Community Atmosphere Model Version 3 (CAM3). The simulated RF at the top of the atmosphere (TOA) is-0.45 W m-2 in the solar spectrum and +0.09 W m-2 in the thermal spectrum on a global average. The magnitude of surface RF is larger than the TOA forcing, with global mean shortwave forcing of-1.76 W m-2 and longwave forcing of +0.31 W m-2 . As a result, dust aerosol causes the absorption of 1.1 W m-2 in t... 相似文献
946.
Influence of the Asian-Pacific Oscillation on Spring Precipitation over Central Eastern China 总被引:2,自引:0,他引:2
The linkage between the Asian-Pacific oscillation(APO)and the precipitation over central eastern China in spring is preliminarily addressed by use of the observed data.Results show that they correlate very well,with the positive(negative)phase of APO tending to increase(decrease)the precipitation over central eastern China.Such a relationship can be explained by the atmospheric circulation changes over Asia and the North Pacific in association with the anomalous APO.A positive phase of APO,characterized by a positive anomaly over Asia and a negative anomaly over the North Pacific in the upper-tropospheric temperature,corresponds to decreased low-level geopotential height(H)and increased high-level H over Asia,and these effects are concurrent with increased low-level H and decreased high-level H over the North Pacific.Meanwhile,an anticyclonic circulation anomaly in the upper troposphere and a cyclonic circulation anomaly in the lower troposphere are introduced in East Asia,and the low-level southerly wind is strengthened over central eastern China.These changes provide advantageous conditions for enhanced precipitation over central eastern China.The situation is reversed in the negative phase of APO,leading to reduced precipitation in this region. 相似文献
947.
西北太平洋区域纬向风垂直切变的变化是影响西北太平洋热带气旋生成和发展的一个重要的动力因子,弱的纬向风切变有利于热带气旋的发生、发展。文中将西北太平洋区域纬向风垂直切变幅度(MWS)定义为850与200 hPa的纬向风之差的绝对值,以研究MWS的气候特征。结果表明,西北太平洋区域的MWS有两个主要空间模态,第1空间模态表现为在15°N以南的热带西太平洋存在MWS东西向变化相反的两个区域,20°N附近的热带西太平洋MWS的变化与其以北海区的MWS的变化相反。第2空间模态表现为在热带太平洋140°E东、西的变化相反。研究了两个模态相关的大气环流特征,发现去掉强ENSO信号后,第1模态不但与低纬度大气环流有关,而且还与南、北半球中高纬度的大气环流有关,第2模态主要与热带西太平洋和北太平洋局地大气环流有关。另外,第1模态的时间系数与赤道东太平洋海温、西北太平洋台风生成频次有着密切联系;第2模态时间系数与西北太平洋台风活动频次联系密切。 相似文献
948.
河北省霾时空分布特征分析 总被引:17,自引:3,他引:14
利用河北省142个气象台站的霾资料,对1971—2007年河北霾的时空分布特征进行了统计分析,发现河北霾出现频数具有明显的地域性和月际分布特征。山麓地区霾平均出现频数最高,明显高于其两侧的平原和山地,山地霾频数最小。霾频数的月际分布特征是12月或1月最多,8月或9月最少。利用2004—2007年500 hPa高度和海平面气压实况资料,通过分析对比,统计归纳出河北地区霾日500 hPa的环流形势有纬向型、两槽一脊型、均值场型、一脊一槽型和两脊一槽型5种。分析结果表明,霾的出现与天气形势有关,霾频数大小与空气污染程度和地形联系密切。这些结果对于了解河北霾的生成机制和预报具有重要意义。 相似文献
949.
采用CAM3(Community Atmosphere Model Version3)模式中海气湍流通量参数化原方案和改进方案,利用观测海温驱动CAM3模式进行气候模拟,以分析模式对厄尔尼诺事件影响气候变化的模拟能力。结果表明,采用CAM3模式海气湍流通量参数化改进方案,模式能够更好地模拟出由厄尔尼诺事件引起的北太平洋和北美地区大气环流的变化,尤其是对厄尔尼诺年冬季阿留申低压强度和与PNA遥相关型有关的500hPa位势高度异常的模拟。 相似文献
950.
Interdecadal change in the connection between Hadley circulation and winter temperature in East Asia 总被引:5,自引:0,他引:5
Based on NCEP/NCAR reanalysis data, the interdecadal variability of Hadley circulation (HC) and its association with East Asian temperature in winter are investigated. Results indicate that the Northern Hemisphere winter HC underwent apparent change in the 1970s, with transition occurring around 1976/77. Along with interdecadal variability of HC, its linkage to surface air temperature (SAT) in East Asia also varied decadally, from weak relations to strong relations. Such a change may be related to the interaction between HC and the atmospheric circulation system over the Philippines, which is associated with the East Asian winter monsoon (EAWM). Before the 1970s, the connection between HC and the anticyclonic circulation around the Philippines was insignificant, but after the late 1970s their linkage entered a strong regime. The intensification of this connection may therefore be responsible for the strong relations between HC and East Asian winter temperatures after the late 1970s. 相似文献