1999 Vol. 18, No. 2
Display Method:
1999, (2): 147-166.
Abstract:
A three-dimensional numerical model of the coastal plume in an ideal basin for the western Gulf of Maine of USA, based on the observations, was configured to examine the dynamical properties under the spring riverine, tidal, and wind forcing.The purp...
A three-dimensional numerical model of the coastal plume in an ideal basin for the western Gulf of Maine of USA, based on the observations, was configured to examine the dynamical properties under the spring riverine, tidal, and wind forcing.The purp...
1999, (2): 167-176.
Abstract:
NOAA AVHRR data from the Bay of Biscay between 1988 and 1990 have been examined in order to extract information on the fluctuations of sea surface temperature (SST) at the diurnal time scale.The temporal and spatial distributions of diurnal warming i...
NOAA AVHRR data from the Bay of Biscay between 1988 and 1990 have been examined in order to extract information on the fluctuations of sea surface temperature (SST) at the diurnal time scale.The temporal and spatial distributions of diurnal warming i...
1999, (2): 177-189.
Abstract:
The Geosat altimeter ERM T2-GDRs data were used to analyze sea surface height (SSH) variabilities in the Northwest Pacific region of 10°-45°N, 120°-160°E covering all the Kuroshio Current.After processing the Geoset GDRs data, the 50 gridded SSH anom...
The Geosat altimeter ERM T2-GDRs data were used to analyze sea surface height (SSH) variabilities in the Northwest Pacific region of 10°-45°N, 120°-160°E covering all the Kuroshio Current.After processing the Geoset GDRs data, the 50 gridded SSH anom...
1999, (2): 191-201.
Abstract:
A baroclinic typhoon model with a moving multi-nested grid is applied in marine environmental forecasts.This paper describes the numerical methods of the model including governing equations, finite differencing, split scheme and time integration.
A baroclinic typhoon model with a moving multi-nested grid is applied in marine environmental forecasts.This paper describes the numerical methods of the model including governing equations, finite differencing, split scheme and time integration.
1999, (2): 203-214.
Abstract:
Based on the reanalysis data of global SOOhPa gcopotential height (NCEP NCAR CDAS-1) and tropical Pacific SSTs, the characteristics of global subtropical highs and their response to tropical eastern Pacific SST are investigated.Results show that glob...
Based on the reanalysis data of global SOOhPa gcopotential height (NCEP NCAR CDAS-1) and tropical Pacific SSTs, the characteristics of global subtropical highs and their response to tropical eastern Pacific SST are investigated.Results show that glob...
1999, (2): 215-223.
Abstract:
A preliminary account of synthetic aperture radar (SAR) imaging mechanisms of oceanic bottom topographic features and a description of the principles of the information extracted from SAR images and the processing and the analysis technology of SAR i...
A preliminary account of synthetic aperture radar (SAR) imaging mechanisms of oceanic bottom topographic features and a description of the principles of the information extracted from SAR images and the processing and the analysis technology of SAR i...
1999, (2): 225-236.
Abstract:
Using the CTD data investigated at about 330 stations in the southern Taiwan Strait, the northeastern South China Sea and their adjacent seas in August and September of 1994, this paper anayses the sectional distributions of salinity in 10 selected s...
Using the CTD data investigated at about 330 stations in the southern Taiwan Strait, the northeastern South China Sea and their adjacent seas in August and September of 1994, this paper anayses the sectional distributions of salinity in 10 selected s...
1999, (2): 237-246.
Abstract:
Based on the CTD data obtained in the southern Taiwan Strait and its adjacent areas in August and September of 1994, the distributional features of the temperature and salinity in the studied area have been analyzed in detail.The results are as follo...
Based on the CTD data obtained in the southern Taiwan Strait and its adjacent areas in August and September of 1994, the distributional features of the temperature and salinity in the studied area have been analyzed in detail.The results are as follo...
1999, (2): 247-255.
Abstract:
Dissolved Cu, Pb, Zn and Cd in the I-Iaikou Bay waters were measured to be respectively in the range concentrations of 0.47-1.16μg/dm3, 0.94-2.36 μg/dm3, 1.28-4.83 μg/dm3 and 0.005-0.072 μg/dm3; with respectively average values of 0.78 μg/dm3, 1.36 μ...
Dissolved Cu, Pb, Zn and Cd in the I-Iaikou Bay waters were measured to be respectively in the range concentrations of 0.47-1.16μg/dm3, 0.94-2.36 μg/dm3, 1.28-4.83 μg/dm3 and 0.005-0.072 μg/dm3; with respectively average values of 0.78 μg/dm3, 1.36 μ...
1999, (2): 257-266.
Abstract:
In order to study the phase transformation between 1nm manganate and 0.7nm mangenate, a series of Slnm Me2+ tnanganates were made after the synthetic lnm Na+ manganate substituted with different kinds of divalent rations.The X-ray diffraction analysi...
In order to study the phase transformation between 1nm manganate and 0.7nm mangenate, a series of Slnm Me2+ tnanganates were made after the synthetic lnm Na+ manganate substituted with different kinds of divalent rations.The X-ray diffraction analysi...
1999, (2): 267-272.
Abstract:
Based on regional compensation and experimental isostasy, the calculating formula of theoretical isostatic response function is deduced when the loads on top correlate with loads from below.A variety of curves of theoretical isostatic response functi...
Based on regional compensation and experimental isostasy, the calculating formula of theoretical isostatic response function is deduced when the loads on top correlate with loads from below.A variety of curves of theoretical isostatic response functi...
1999, (2): 273-278.
Abstract:
Based on regional compensation model and experimental isostasy, the isostatic response function of the Okinawa Trough is calculated by using gravity and topographic data.The results are shown as follows:the effective elastic thickness of the plate an...
Based on regional compensation model and experimental isostasy, the isostatic response function of the Okinawa Trough is calculated by using gravity and topographic data.The results are shown as follows:the effective elastic thickness of the plate an...
1999, (2): 279-291.
Abstract:
