全文获取类型
收费全文 | 337篇 |
免费 | 78篇 |
国内免费 | 85篇 |
专业分类
测绘学 | 17篇 |
大气科学 | 228篇 |
地球物理 | 111篇 |
地质学 | 62篇 |
海洋学 | 28篇 |
天文学 | 17篇 |
综合类 | 10篇 |
自然地理 | 27篇 |
出版年
2023年 | 2篇 |
2022年 | 10篇 |
2021年 | 6篇 |
2020年 | 18篇 |
2019年 | 15篇 |
2018年 | 9篇 |
2017年 | 17篇 |
2016年 | 16篇 |
2015年 | 20篇 |
2014年 | 21篇 |
2013年 | 27篇 |
2012年 | 29篇 |
2011年 | 35篇 |
2010年 | 12篇 |
2009年 | 27篇 |
2008年 | 27篇 |
2007年 | 23篇 |
2006年 | 24篇 |
2005年 | 16篇 |
2004年 | 15篇 |
2003年 | 8篇 |
2002年 | 14篇 |
2001年 | 13篇 |
2000年 | 11篇 |
1999年 | 12篇 |
1998年 | 17篇 |
1997年 | 13篇 |
1996年 | 10篇 |
1995年 | 5篇 |
1994年 | 4篇 |
1993年 | 6篇 |
1992年 | 5篇 |
1991年 | 4篇 |
1990年 | 4篇 |
1989年 | 3篇 |
1986年 | 1篇 |
1983年 | 1篇 |
排序方式: 共有500条查询结果,搜索用时 15 毫秒
1.
Stable oxygen isotope analysis and measurement of several dissolved cations and anions of bulk meltwater samples have provided information about the hydrochemical environment of the glacial hydrological system at Imersuaq Glacier, an outlet tongue from the Greenland ice‐sheet, West Greenland. The samples were collected at frequent intervals during the period 20–28 July 2000 in a small (<20 L s?1) englacial meltwater outlet at the glacier margin. The results document the following findings: (i) a marked diurnal variation of δ18O is related to the composition of oxygen isotope provenances, mainly near‐marginal local superimposed ice and basal up‐sheared ice further up‐glacier; (ii) a relationship is seen between all base cations (Na+, K+, Ca2+, Mg2+), SO42? and δ18O, indicating that solute acquisition is provided by solid–solution contact with the up‐sheared ice—as the relationship with Cl? is weak the influence of seasalt‐derived solutes is small in the area; (iii) when the melt rate is high, two diurnal maxima of δ18O values and solute concentrations are measured, and it is suggested that a snow meltwater component is responsible for the second maximum of δ18O—a short residence time leads to a delayed decrease in ion concentrations. Copyright © 2003 John Wiley & Sons, Ltd. 相似文献
2.
本文根据1960~1994年千里岩和青岛月平均气温资料,分析了千里岩与青岛35年来气温的年、季变化特征及差别,发现35年来,千里岩和青岛的年、季平均气温均呈变暖趋势,但千里岩增温幅度较青岛小。从分析中发现,与气温变暖趋势相对应,西北太平洋副热带高压(以下简称副高)面积、强度指数的年、季变化也呈明显的增强、增大趋势。且年平均气温与冬季副高面积指数相关最显著。最后依此关系建立回归方程,并预测了1996年千里岩年平均气温的变化趋势。 相似文献
3.
西太平洋暖池区气象学特征分析 总被引:1,自引:0,他引:1
本文根据TOGA-COARE强化观测资料及卫星资料分析讨论了西太平洋暖池区11-2月间海面气象要素的平均特征。分析发现海面气压平均日变化似乎同中纬度区明显不同。文中还分析讨论了在西太暖池区西风爆发、赤道浅涡、信风逆温及ITCE和南太平洋辐合带SPCZ的变化特征。 相似文献
4.
5.
Estimating groundwater evapotranspiration rates using diurnal water-table fluctuations in a semi-arid riparian zone 总被引:2,自引:1,他引:1
Laura K. Lautz 《Hydrogeology Journal》2008,16(3):483-497
In semi-arid climates, phreatophytes draw on shallow aquifers, and groundwater evapotranspiration (ETG) is a principal component of groundwater budgets. Diurnal water table fluctuations, which often are a product of ETG, were monitored in the riparian zone of Red Canyon Creek, Wyoming, USA. These fluctuations were higher in a riparian wetland (2–36 mm) than a grass-covered meadow (1–6 mm). The onset and cessation of water-table fluctuations correspond to daily temperatures relative to freezing. Spatial differences were due to vegetation type and specific yield, while temporal changes were due to vegetation dormancy. Ratios of ETG to potential evapotranspiration (PET), K c,GW, were similar to ratios of actual evapotranspiration (ET) to PET, K c, in semi-arid rangelands. Before vegetation senescence, K c,GW increased between precipitation events, suggesting phreatophytes pull more water from the saturated zone as soil moisture decreases. In contrast, K c decreases with soil moisture following precipitation events as ET becomes increasingly water-limited. Error in ETG is primarily from estimates of specific yield (S y), which is difficult to quantify in heterogeneous sediments. ETG values may be more reliable because the range of acceptable S y is smaller than K c and S y does not change with vegetation type or soil moisture. 相似文献
6.
7.
青藏高原近地面层微气象学特征 总被引:12,自引:3,他引:12
Liu Huizhi Zhang Hongsheng Bian Lin'gen Chen Jiayi Zhou Mingyu Xu Xiangde Li Shiming Zhao Yijun 《大气科学进展》2002,19(1):73-88
利用1998年5月-7月在改则、当雄和昌都三测站获得的近地面层气象要素变化的观测资料,分析了青藏高原近地面层风速、温度和湿度日变化特征及廓线规律,发现高原近地面层微气象学特征具有自己的特点;同时还讨论了高原近地面层白天出现的逆湿现象。 相似文献
8.
9.
陕西省夏季降水量的长期变化趋势 总被引:3,自引:0,他引:3
对榆林、西安、汉中夏季降水量的历年变化进行分析,并用灰色拓扑方法作了趋势预测。分析表明,关中的初夏旱和伏旱突出,半湿润地区的西安夏季多年平均降水量比半干旱地区的榆林还少。自1951年以来,陕西省夏季降水量的总趋势是:关中、陕南有下降趋势,而陕北下降趋势不明显。另外,关中、陕南的夏季降水还存在连续几年多雨或连续几年少雨的时段,而陕北则呈现出少雨年和多雨年交替出现的高频振荡。 相似文献
10.
In a survey in Greece from 1987 to 2000 hepatotoxic cyanobacterial blooms were observed in 9 out of 33 freshwaters. Microcystins (MCYSTs) were detected by HPLC in 7 of these lakes, and the total MCYST concentration per scum dry weight ranged from 50.3 to 1638 ± 464 μg g—1. Cyanobacterial genera (Microcystis, Anabaena, Anabaenopsis, Aphanizomenon, Cylindrospermopsis) with known toxin producing taxa were present in 31 freshwaters. From our data and a review of the literature, it would appear that Mediterranean countries are more likely 1) to have toxic cyanobacterial blooms consisting of Microcystis spp. and 2) to have higher intracellular MCYST concentrations. A case study in Lake Kastoria is used to highlight seasonal patterns of cyanobacterial and MCYST‐LR occurrence and to assess cyanotoxin risk. Cyanobacterial biovolume was high (> 11 μL L—1) throughout the year and was in excess of Guidance Level 2 (10 μL L—1) proposed by WHO for recreational waters and Alert Level 2 for drinking water. Further, surface water samples from April to November exceeded Guidance Level 3, with the potential for acute cyanobacterial poisoning. Intracellular MCYST‐LR concentrations (max 3186 μg L—1) exceeded the WHO guideline for drinking water (1 μg L—1) from September to November with a high risk of adverse health effects. Preliminary evidence indicates that in 3 lakes microcystins are accumulated in some aquatic organisms. Generally, a high risk level can be deduced from the data for the Mediterranean region. 相似文献