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481.
C. Debi Prasad 《Solar physics》1995,159(1):181-190
A study of existing observations and theoretical concepts about the circumsolar emission in infrared radiation and its relation to the dust ring have been carried out. It is shown that the dust ring is temporally variable and depends on the solar cycle - being easily observable during minimum phase of the solar activity. Its constituent must be fine particles, instead of 10 km sized boulders at 4R from the Sun. It is also shown that the measurement along the coronal features such as streamers give rise to higher flux estimates. 相似文献
482.
Summary Active weak and break phases of the Indian summer monsoon for the period 1958–2002 are studied using ERA-40 data. The criteria
for identifying the break are proposed and tested using the 850 hPa level horizontal wind shear. Independent datasets such
as All-India Rainfall, NOAA Outgoing Long-wave Radiation and CMAP rainfall datasets are used for the verification of the proposed
criteria.
On leave from the National Center for Medium Range Weather Forecasting, A-50 Institutional Area, Phase-II, Sector 62, Noida,
U.P., India. 相似文献
483.
The second campaign of the Arabian Sea Monsoon Experiment (ARMEX-II) was conducted in two phases viz., March–April and May–June
2003. In the present work, the buoy and ocean research vessel data collected during the second phase of ARMEX-II have been
analysed to bring out the characteristic features of monsoon onset. The results have shown that the thermodynamical features
such as build up of lower tropospheric instability and increased height of zero degree isotherm occurred about a week before
the monsoon onset over Kerala and adjoining southeast Arabian Sea. There was a sharp fall in the temperature difference between
850 and 500 hPa, and the height of zero degree isotherm about 2–3 days before the monsoon onset. The flux of sensible heat
was positive (sea to air) over south Arabian Sea during the onset phase. Over the Bay of Bengal higher negative (air to sea)
values of sensible flux prevailed before the monsoon onset which became less negative with the advance of monsoon over that
region.
The pre-onset period was characterized by large sea surface temperature (SST) gradient over the Arabian Sea with rapid decrease
towards north of the warm pool region. The buoy observations have shown that SST remained close to 30.5°C in the warm pool
region during the pre-onset period in 2003 but only 2–3 degrees away (north of this region) SSTs were as low as 28.5–29°C.
An interesting aspect of sea level pressure (SLP) variability over the Indian seas during the onset phase of summer monsoon
2003 was undoubtedly, the highest SLP in the warm pool region inspite of very high SSTs. 相似文献
484.
V. K. Prasad 《The Photogrammetric Record》2006,21(116):414-415
485.
Anup K. Prasad Lim Chai Ramesh P. Singh Menas Kafatos 《International Journal of Applied Earth Observation and Geoinformation》2006
Numerous efforts have been made to develop various indices using remote sensing data such as normalized difference vegetation index (NDVI), vegetation condition index (VCI) and temperature condition index (TCI) for mapping and monitoring of drought and assessment of vegetation health and productivity. NDVI, soil moisture, surface temperature and rainfall are valuable sources of information for the estimation and prediction of crop conditions. In the present paper, we have considered NDVI, soil moisture, surface temperature and rainfall data of Iowa state, US, for 19 years for crop yield assessment and prediction using piecewise linear regression method with breakpoint. Crop production environment consists of inherent sources of heterogeneity and their non-linear behavior. A non-linear Quasi-Newton multi-variate optimization method is utilized, which reasonably minimizes inconsistency and errors in yield prediction. 相似文献
486.
487.
Geomorphic characterization and diversity of the fluvial systems of the Gangetic Plains 总被引:2,自引:0,他引:2
The extensive Gangetic alluvial plains are drained by rivers which differ strongly in terms of hydrological and sediment transport characteristics. These differences are manifested in the geomorphic diversity of the plains. The Western Gangetic Plains (WGP) are marked by a degradational topography with incised channels and extensive badland development in some parts, while the Eastern Gangetic Plains (EGP) are characterized by shallow, aggrading channels with frequent avulsions and extensive flooding. We interpret such geomorphic diversity in terms of differences in stream power and sediment supply from the catchment areas. The rivers draining the western plains are marked by higher stream power and lower sediment yield that result in degradation. In comparison, the rivers draining the eastern Gangetic Plains have lower stream power and higher sediment yield that result in aggradation. The variation of stream power, a function of channel slope and high sediment yield, is attributed to differences in rainfall and rate of uplift in the hinterland. It is suggested that such differences have resulted in a marked geomorphic diversity across the plains. It is also suggested that such diversity has existed for a fairly long time because of climatic and tectonic variance. 相似文献
488.
Anup K. Prasad Ramesh P. Singh Ashbindu Singh 《Journal of the Indian Society of Remote Sensing》2004,32(4):313-316
High AOD is observed over the Ganga basin throughout the year unlike southern India, is alarming as this basin is one of the
most productive basins of Indian subcontinent having population of more than 460 million. AOD is found to be increasing rapidly
since 2000 in summer season that may cause adverse effect to the agricultural crops and also to the human health. Increased
aerosol loading may likely affect the rainfall which is responsible for the observed drought conditions over the Indian subcontinent.
Detailed analysis of AOD, crop yields and rainfall data are required to understand the impact of increasing aerosol loading
over the Indian subcontinent. 相似文献
489.
A third generation wave prediction model (WAM) suitably modified for the Indianseas was used to simulate the sea state during typical monsoon months of July 1987,88 and 89. During July 1987, small-scale disturbances over the Arabian Sea and theBay of Bengal as reported from earlier works were noticed in the wave hindcast. Thegridded monthly averaged wave heights for the above periods were compared with theGEOSAT altimeter data. A comparison between model computed wave parameters andavailable ship observations was also carried out for July 1987, 88 and 89.The modelwas run with ECMWF analyzed wind field for a period of one month. The comparisonshowed that the wave heights from the model matches with those from GEOSATAltimeter and ships of opportunity. 相似文献
490.
V Krishna Prasad T Rajagopal Yogesh Kant Surya Srinivas K S Badarinath 《Journal of the Indian Society of Remote Sensing》1998,26(3):103-112
Present study attempts to utilise the spatial information from IRS-IC LISS-III satellite data, through, tie use of Semivartogram apprqatfu for analyzing the overstorey. diversity In forest stands, Semivariance has been calculated for all the pixels in I5x15 pixel window for each of the forest stand using digital numbers from near infrared channel Variation in semivariance has been correlated to stand density and species composition. Analysis of averaged semivariance for overall diversity of forest stands suggested, decreasing semi variance in the order, mixed dry (feciduous forests, mixed scrub forests followed by dry deciduous forest Semivariance has been found to be highly Correlated to tree density (R2 = 0.96) suggesting semivariograms as one of the measures for studies on tree density, canapy cover and diversity patterns. 相似文献