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   145篇
  免费   7篇
  国内免费   6篇
大气科学   2篇
地球物理   35篇
地质学   23篇
海洋学   70篇
天文学   1篇
综合类   4篇
自然地理   23篇
  2023年   1篇
  2022年   2篇
  2019年   3篇
  2018年   2篇
  2017年   4篇
  2016年   2篇
  2015年   5篇
  2014年   12篇
  2013年   8篇
  2012年   5篇
  2011年   7篇
  2010年   7篇
  2009年   7篇
  2008年   14篇
  2007年   8篇
  2006年   6篇
  2005年   5篇
  2004年   10篇
  2003年   4篇
  2002年   6篇
  2001年   4篇
  2000年   7篇
  1999年   4篇
  1998年   2篇
  1997年   2篇
  1996年   1篇
  1995年   5篇
  1994年   4篇
  1992年   2篇
  1990年   2篇
  1987年   2篇
  1986年   2篇
  1982年   2篇
  1981年   1篇
排序方式: 共有158条查询结果,搜索用时 15 毫秒
101.
印度洋金枪鱼延绳钓渔业作为我国重要的远洋渔业之一,探究其渔场时空变动及与环境因子之间的关系十分必要。本文根据2016年1—6月收集的印度洋金枪鱼渔业生产数据,并结合卫星遥感获取的环境因子数据,运用ArcGIS和GAM模型分析了印度洋大眼金枪鱼和黄鳍金枪鱼渔场时空变动及与环境因子之间的关系。研究结果表明:大眼金枪鱼和黄鳍金枪鱼1—6月CPUE均呈现先减小后增加的趋势,4月均达最高值,分别为2.45尾/千钩和3.56尾/千钩,各月CPUE均存在显著性差异(P<0.001);大眼金枪鱼和黄鳍金枪鱼渔场时空变动基本趋于一致,均为先向东北移动,后向西北移动,最后再向东北移动的趋势;GAM模型分析显示,大眼金枪鱼CPUE与模型因子的解释率为32.1%,纬度和250 m水深温度影响最显著,黄鳍金枪鱼CPUE与模型因子的解释率为37.2%,200 m水深温度影响最显著;协同分析表明,1—6月,印度洋金枪鱼延绳钓中心渔场分布于1°S~9.5°N,47°~64°E,且海表温度在29.3~30.8℃的海域。  相似文献   
102.
海洋调查船是了解认知与开发利用海洋的关键基础设施。欧洲海洋调查船运作组织(ERVO)推动这一关键基础设施协同的努力颇具代表性。它面对欧洲海洋调查船多元化且无权威主体的境地,通过会员制构建协同平台,明晰了业务主导、可持续发展的协作目标;它通过年会聚焦海洋调查船及相关仪器装备,交流运行管理,研讨技术创新、改造更新以及与海洋调查船相关的共性话题,以促进欧洲海洋调查船和相关装备具有最佳的运行成效;它与相关海洋调查与研究组织机构联动,跻身于欧洲海洋调查船发展战略层,推动欧洲海洋调查船在项目层面组队共享。文章解析了欧洲海洋调查船运作组织的背景和运作模式,同时针对我国海洋调查船协作多头发力缺乏合纵连横的状况,提议发起中国海洋调查船协同论坛,组建联合工作组做好长期务实的基础性工作,筹划中国及关系国调查船协调计划,以建立我国海洋调查船协同机制并逐步跻身国际海洋调查船战略协同层。  相似文献   
103.
《自然地理学》2013,34(1):76-96
Regions based on seasonal precipitation variability for Hawaii are determined using a principal components analysis applied to 124 stations for the period 1971-2000. Nine regions are delineated and are consistent with known precipitation patterns; leeward and windward stations are in separate regions on all islands. Within each region, the relationship between precipitation and the El Niño-Southern Oscillation (ENSO) is examined using a correlation analysis with the Southern Oscillation Index (SOI), and the Niño 3.4 and Niño 1+2 indices. Precipitation is most frequently correlated with ENSO in the different regions using SOI and Niño 3.4. Using several nonparametric statistical tests, it is determined that while average precipitation received in Hawaii during El Niño events is significantly different from average precipitation (1971-2000) and from precipitation received during La Niña events, the relationship between precipitation and individual ENSO events within regions is rarely significant. Finally, during El Niño or La Niña events, average precipitation receipt across the regions co-varies during winter and summer under concurrent conditions and a one-season lag. Synoptic patterns are examined and indicate a deviation from average conditions during ENSO events that affects subsidence and precipitation patterns.  相似文献   
104.
Interception losses in stands of non‐native trees in Hawaiian forests and their potential negative impacts on fresh water availability are poorly understood. In this study, a canopy water balance analysis was conducted to estimate interception losses using measurements of rainfall (RF), throughfall (TF), and stemflow (SF) at three locations, each dominated by one or more of the following non‐native tree species: Psidium cattleianum Sabine (Strawberry guava), Schinus terebinthifolius Raddi (Christmas berry), Syzygium cumini (L.) Skeels (Java plum), and Coffea arabica L. (Coffee). Mean TF expressed as percentage of total RF was the lowest (43.3%) under a monotypic stand of P. cattleianum and the highest (56.5%) under mixture of S. terebinthifolius, P. cattleianum, and S. cumini. Observed SF was highest (33.9%) under P. cattleianum and lowest (3.6%) under a mixture of S. terebinthifolius, P. cattleianum, and S. cumini. The relatively high SF under P. cattleianum can be attributed to its smooth bark, stem density, and steep branching. The mean observed canopy interception varied between 23% under P. cattleianum and 45% at the site dominated by C. arabica. Mean direct TF coefficients from individual events at each location ranged from a low of 0.36 under the canopy dominated by C. arabica to a high of 0.51 under the canopy dominated by S. terebinthifolius, P. cattleianum, and S. cumini. In contrast, the mean SF partitioning coefficients from individual storm events at each location ranged from a low of 0.05 under the canopy dominated by S. terebinthifolius, P. cattleianum, and S. cumini to a high of 0.37 under P. cattleianum. Mean canopy storage capacity was highest (1.90) at the site dominated by S. terebinthifolius, P. cattleianum, and S. cumini whereas trunk storage capacity was highest (0.54) under the P. cattleianum. Copyright © 2012 John Wiley & Sons, Ltd.  相似文献   
105.
We investigated the physical properties of beaches contaminated with plastic fragments. We compared sediment cores from Hawai‘i Island’s Kamilo Beach, notable for plastic accumulation, to cores from a nearby beach. Compared to the nearby beach, Kamilo sediments contained more plastics (up to 30.2% by weight), were coarser-grained, and were more permeable (t-test, p < 0.0001). 85% of the fragments were polyethylene, and 95% were concentrated in the top 15 cm of the cores. We constructed artificial cores of standardized grain size and varying plastic-to-sediment ratios. Adding plastic significantly increased the permeability (ANOVA, p = 0.002), which was partially attributed to the fragments increasing the mean grain size. Sediments with plastic warmed more slowly (16% maximum decrease in thermal diffusivity), and reached lower maximum temperatures (21% maximum increase in heat capacity). These changes have a variety of potential effects on beach organisms, including those with temperature-dependent sex-determination such as sea turtle eggs.  相似文献   
106.
Fish stocks associated with seamounts may be particularly susceptible to overexploitation. From January to July 2001, the Spanish Oceanographic Institute (IEO) conducted an experimental fishing survey entitled ‘Palguinea-2001’ on the seamounts of the Sierra Leone Rise. Beryx splendens (commonly called alfonsino) is the main commercial demersal fish associated with this area. The aim of this study was to investigate the effects of a demersal longline fishery targeting B. splendens on the previously unexploited small Machucambo Seamount over a short time-scale, and also to consider trends in pooled catch rate at another four seamounts. During 110 fishing days at Machucambo, a total catch of 207 tonnes of B. splendens was taken with a fishing effort of 1 309 070 hooks. A spectral analysis and red-noise spectra procedure (REDFIT) algorithm was used to identify the red-noise spectrum from the gaps in the observed time-series of catch per unit effort by weight. Our results show the potential impact of longline fishing pressure on an unexploited ecosystem – after approximately 50 fishing days, the stock appeared to decline substantially, as reflected by a marked drop in catch per unit effort. The apparent rapid decline of the stock might be related to the small size and the virgin state of the Sierra Leone seamounts. The results could be extrapolated to similar small seamounts elsewhere.  相似文献   
107.
108.
The normal to reverse Lower Mammoth reversal (3.33 Ma) has been recorded in several sequences of lava from the Waianae Volcano, the Island of Oahu, Hawaii. 137 samples from 29 flows from the Pu'u Paheehee section have been the subject of a palaeointensity study using the microwave technique. Duplicate sister samples from the directional study of Herrero-Bervera and Valet (Earth Planet. Sci. Lett. 171 (1999) 139–148) were used. Microwave demagnetisation was carried out on all samples and the directions compared to the published flow mean directions. Microwave palaeointensity experiments were carried out on all accepted samples using the 8.2 GHz and 14 GHz microwave systems. The perpendicular applied field palaeointensity method and a Coe analogue method were used. Eighty-four samples from 24 flows gave acceptable palaeointensity results. The results indicate that the geomagnetic field was low (mean 5.9±1.3 μT (N=7)) prior to the transitional directions. During the first stage of the reversal the field remains low. Results however could only be obtained from three transitional flows. The field then strongly recovers with very high intensity (70 μT) and reversed direction. After this the intensity decreases before the field becomes transitional again for a cluster of four flows. The field does not reduce as much as previously, rather it is about twice the pre reversal intensity. For the final section of reversed flows the intensity is more than twice the pre reversal mean value, 15.1±5.9 μT (N=7). Whilst some similarities are seen between this reversal and other reversals of different ages and locations there is not enough data at present to say whether there is any systematic behaviour.  相似文献   
109.
The ∼0.2 mm/yr uplift of Hawaiian islands Lanai and Molokai and Hawaiian swell topography pose important constraints on the structure and dynamics of mantle plumes. We have formulated 3-D models of mantle convection to investigate the effects of plume-plate interactions on surface vertical motions and swell topography. In our models, the controlling parameters are plume radius, excess plume temperature, and upper mantle viscosity. We have found that swell height and swell width constraints limit the radius of the Hawaiian plume to be smaller than 70 km. The additional constraint from the uplift at Lanai requires excess plume temperature to be greater than 400 K. If excess plume temperature is 400 K, models with plume radius between 50 and 70 km and upper mantle viscosity between 1020 and 3×1020 Pa s satisfy all the constraints. Our results indicate that mantle plume in the upper mantle may be significantly hotter than previously suggested. This has important implications for mantle convection and mantle melting. In addition to constraining plume dynamics, our models also provide a mechanism to produce the observed uplift at Lanai and Molokai that has never been satisfactorily explained before.  相似文献   
110.
The objective of this paper is to identify water-flow patterns in part of an active landslide, through the use of numerical simulations and data obtained during a field study. The approaches adopted include measuring rainfall events and pore-pressure responses in both saturated and unsaturated soils at the site. To account for soil variability, the Richards equation is solved within deterministic and stochastic frameworks. The deterministic simulations considered average water-retention data, adjusted retention data to account for stones or cobbles, retention functions for a heterogeneous pore structure, and continuous retention functions for preferential flow. The stochastic simulations applied the Monte Carlo approach which considers statistical distribution and autocorrelation of the saturated conductivity and its cross correlation with the retention function. Although none of the models is capable of accurately predicting field measurements, appreciable improvement in accuracy was attained using stochastic, preferential flow, and heterogeneous pore-structure models. For the current study, continuum-flow models provide reasonable accuracy for practical purposes, although they are expected to be less accurate than multi-domain preferential flow models. Electronic Publication  相似文献   
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