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81.
联合气压测高定位的高程转换问题 总被引:1,自引:0,他引:1
针对利用联合气压测高技术进行导航定位时,直接测量获得的用户海拔高与定位解算中所需的大地高容易被混淆的问题,该文提出将气压基准站作为水准重合点,向用户传输高程异常值以进行高程转换;或在区域范围内建立局域坐标系,直接获得Z坐标值,并进行降维定位解算。这两种方法能够适用于不同情况,解决了气压测高应用范围与测量精度之间的矛盾。最后,通过在校园网中进行的实测实验,对方法进行了验证。结果表明,本方法可以较好地消除高程差异,有效提高定位精度。 相似文献
82.
By combining Argos drifter buoys and TOPEX/POSEIDON altimeter data, the time series of sea-surface velocity fields in the
Kuroshio Current (KC) and adjacent regions are established. And the variability of the KC from the Luzon Strait to the Tokara
Strait is studied based on the velocity fields. The results show that the dominant variability period varies in different
segments of the KC: The primary period near the Luzon Strait and to the east of Taiwan Island is the intra-seasonal time scale;
the KC on the continental shelf of the ECS is the steadiest segment without obvious periodicity, while the Tokara Strait shows
the period of seasonal variability. The diverse periods are caused by the Rossby waves propagating from the interior ocean,
with adjustments in topography of island chain and local wind stress.
Supported by the National Basic Research Program of China (973 Program, Nos. 2007CB411804, 2005CB422303), the NSFC (No. 40706006),
the Key Project of International Science and Technology Cooperation Program of China (No. 2006DFB21250) and the “111 Project”
(B07036), the Program for New Century Excellent Talents in University (NECT-07-0781) 相似文献
83.
84.
J. A. Kamalakar K. V. S. Bhaskar A. S. Laxmi Prasad R. Ranjith K. A. Lohar R Venketeswaran T. K. Alex 《Journal of Earth System Science》2005,114(6):725-731
Lunar Laser Ranging Instrument (LLRI) proposed for the first Indian lunar mission Chandrayaan-1 is aimed to study the topography
of the Moon’s surface and its gravitational field by precisely measuring the altitude from a polar orbit around the Moon.
Altimetry data close to the poles of the Moon would also be available from the instrument, which was not covered by earlier
missions. This instrument supplements the terrain mapping camera and hyperspectral imager payloads on Chandrayaan-1. The instrument
consists of a diode pumped Nd:YAG pulsed laser transmitter having 10 nsec pulse width and a receiver system. The receiver
system features 17 cm diameter Ritchey—Chrétien collecting optics, Si Avalanche Photo Detector (APD), preamplifiers, constant
fraction discriminators, time-of-flight measurement unit and spacecraft interface. Altimeter resolution of better than 5 m
is targeted. The received signal strength of LLRI depends on laser pulse backscatter from the Moon’s surface. Moon’s surface
being a poor reflector, the choice of receiver size and its type and the selection of detector play an important role in getting
a good signal-to-noise ratio and in turn achieving the target resolution. At the same time, the spacecraft puts a limitation
on payload size and weight. This paper discusses the proposed LLRI system for Chandrayaan-1 and signal-to-noise ratio estimation. 相似文献
85.
Coastal Gravity Anomalies from Retracked Geosat/GM Altimetry: Improvement, Limitation and the Role of Airborne Gravity Data 总被引:6,自引:0,他引:6
Cheinway Hwang Jinyun Guo Xiaoli Deng Hsin-Ying Hsu Yuting Liu 《Journal of Geodesy》2006,80(4):204-216
We process geophysical and waveform data records of the Geosat/GM (geodetic mission) satellite altimeter mission for waveform retracking and applications. An improved threshold retracker is developed. The performances of the Beta-5, threshold and improved threshold retrackers are assessed over waters around Taiwan. The improved threshold retracker outperforms the other two. The improvement in the accuracy of sea surface height (SSH) is investigated according to marine zone and the distance of waters to the shore. The improvement rate increases closer to the land, with the largest improvement rate of about 20% in waters within 10 km of the shore. Over waters around islands and coasts, there are still retracked SSHs with large errors. Least-squares collocation is used to compute gravity anomalies from the Geosat/GM altimeter data. Use of retracked SSHs improves the accuracy of gravity anomalies by about 11%. Adding airborne gravity data further improves the accuracy, especially in the immediate vicinity of the coasts. Tide model errors over coastal waters remain a problem in altimetry applications, even if the waveforms are properly retracked. 相似文献
86.
Geosat/GM波形重跟踪反演中国沿海区域重力异常 总被引:1,自引:1,他引:0
利用Geosat/GM测高波形数据,在中国海域内(117°E~129°E,21°N~41°N)比较了阈值法、Beta5和改进阈值法三种重跟踪算法.分析表明,改进阚值法优于其他两种重跟踪方法.由改进阈值法的测高数据.分别采用最小二乘法(least sqlilare collocation,LSC)和逆Vening-Meinesz(IVM)计算了卫星测高重力异常,并与船测重力数据进行了比较.结果显示,LSC的精度优于IVM.与KMS02和Sandwell & Smith V15两个重力场模型相比较,本文结果在东海优于这两个模型,在台湾海域结果稍差,需要融合ERS-1等其他数据进一步提高精度. 相似文献
87.
88.
89.
Ute C. Herzfeld Craig S. Lingle Cecily Freeman Chris A. Higginson Michael P. Lambert Li-Her Lee Vera A. Voronina 《Mathematical Geology》1997,29(7):859-890
The Antarctic Ice Sheet plays a major role in the global system, and the large ice streams discharging into the circumpolar sea represent its gateways to the world's oceans. Satellite radar altimeter data provide an opportunity for mapping surface elevation at kilometer-resolution with meter-accuracy. Geostatistical methods have been developed for the analysis of these data. Applications to Seasat data and data from the Geosat Exact Repeat Mission indicate that the grounding line of Lambert Glacier/Amery Ice Shelf, the largest ice stream in East Antarctica, has advanced 10–12 km between 1978 and 1987–89. The objectives of this paper are to explore possibilities and limitations of satellite-altimetry-based mapping to capture changes for shorter time windows and for smaller areas, and to investigate some methodological aspects of the data analysis. We establish that one season of radar altimeter data is sufficient for constructing a map. This allows study of interannual variation and is the key for a time-series analysis approach to study changes in ice streams. Maps of the lower Lambert Glacier and the entire Amery Ice Shelf are presented for austral winters 1978, 1987, 1988, and 1989. As a first step toward understanding the dynamics of the ice-stream/ice-shelf system, elevation changes are calculated for grounded ice, the grounding zone, and floating ice. In the absence of (sufficient) surface gravity control for the Lambert Glacier/Amery Ice Shelf area, altimetry-based maps may facilitate improvement of geoid models as they provide constraints on the terrain correction in the inverse gravimetric problem. 相似文献
90.
中国近海1992~1998海平面变化监测与分析 总被引:14,自引:1,他引:13
利用Topex/Poseidon和ERS-1卫星测高资料采用“共线”法计算出1992-10~1998-06中国近海海域海平面及其变化。在扣除T/P卫星测高仪的零点漂移影响后,发现与全球海平面上升率(+2.1±1.3)mm/a相比,不同海域的海平面变化趋势大不相同,黄、东、南海的海平面年变化率分别为:(+3.44±0.61)mm/a,(+3.12±0.47)mm/a,(-1.41±0.48)mm/a。从海平面变化异常中可以看出1993,1994,1997~1998年3次El Nino异常对中国近海海域海平面的影响是南海海域最大,东海次之,黄海最小。除了对海平面进行传统的频谱分析外,还进行了多分辨率的小波分析,还发现在上述3个海域中除了年周期变化较为稳定外,半年及季节(100 d)周期项存在着时间漂移。此外,在上述3个海域还存在着明显的两个月(62 d)周期的变化,其激发原因在此做了初步探讨。 相似文献