THE INFLUENCE OF INTERACTION BETWEEN SHIFT OF WARM POOL AND THAT OF THE EQUATORIAL CONVERGENCE ZONE ON ATMOSPHERIC SURFACE WIND FIELDS DURING 1982/83 ENSO
THE INFLUENCE OF INTERACTION BETWEEN SHIFT OF WARM POOL AND THAT OF THE EQUATORIAL CONVERGENCE ZONE ON ATMOSPHERIC SURFACE WIND FIELDS DURING 1982/83 ENSO
The chondroitin-sulfate microenvironment made the enzyme resistant to heparin inhibition because the equatorial orientation of the OH groups is similar to that in hyaluronic acid.
例句来源
Near-Equatorial Electrons as Measured onboard the MirSpace Station
例句来源
Some results of studying the electrons with energies of tens to hundreds of keV at the low and near- equatorial geomagnetic latitudes by using the instruments Sprut-V and Ryabina-2 onboard the Mirspace station in 1991 are presented.
例句来源
The most intense electron fluxes are observed at the lower edge of the near-equatorial boundary of the inner radiation belt on longitudes of the South Atlantic Anomaly between 14 and 20 h MLT.
例句来源
The motion of a spherically symmetric balloon satellite near the equatorial plane is considered.
This is a brief report of a preliminary survey of certain rain-bearing systems over China in later spring and summer. In the first part, a general description of the methods of analysis used in this survey is given. As the temperature and wind fields are weak, and the precipitation is heavy, smaller intervals for the isotherms and contours in the constant pressure surface and pseudo-equivalent potential instead of potential temperature in the cross section analysis are used.In the second part, there are des...
Utilizing the latitudinal mean ot upper meridional wind of 1950 given by Buch and Starr and White, mean meridional circulation has been studied. Fig. 1-3 (fig. 1 for whole year, fig. 2 for winter, fig. 3 for summer) reveal three cells: two direct cells in low and high latitudes respectively and one indirect cell in middle latitudes. The average jet stream of 1950 is situated in the middle cell. The yearly average equatorial convergence zone is at about 5°N. From winter to summer all the three cells sh...
During summer very often there is a heavy-rain bearing west-east shear line in the lower troposphere over Yangtze-Hwai valley. To the north of the shear line, the wind is predominantly from east or northeast, and to the south from the west or southwest. Its appearance is most evident on 850 and 700 mb surface.In this paper a case study of this type of shear line is made. It is shown that the dynamical and thermal effects of Tibet plateau is the one of the important factors for its formation.The analysis of ...