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tropical ocean area
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  热带海域
     OBSERVATION RESEARCH OF THE TURBULENT FLUXES OF MOMENTUM, SENSIBLE HEAT AND LATENT HEAT OVER THE WEST PACIFIC TROPICAL OCEAN AREA
     西太平洋热带海域动量、感热和潜热等湍流通量的观测研究
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  “tropical ocean area”译为未确定词的双语例句
     The results show that for this tropical ocean area the drag coefficient CD is equal to (1.53±0.25) × 10-3, and the daily mean latent flux HL is greater than its daily mean sensible flux Hs, by factor of about 9.
     结果表明,这一海域上的曳力系数值C_D=(1.53±0.25)×10~(-3); 该海域总是将其贮存的热量以感热形式特别是以潜热形式输送到大气中(其中感热输送仅占10%,其余主要为水汽潜热输送),使该海域成为地球上不可多见的热源。
短句来源
  相似匹配句对
     ASYMMETRY OF UNSTABLE WAVES IN THE TROPICAL OCEAN
     热带海洋中非稳定波的不对称现象(英文)
短句来源
     Simulation of Seasonal Variations in the Tropical Pacific Ocean
     热带太平洋环流季节变化的数值模拟
短句来源
     Ocean's Eleven
     《十一罗汉》(英文)
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     OCEAN WORLD
     广州海洋馆
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     The Relationship between OLR in Tropical Ocean Areas and Summer Rainfall in Shandong and Its Forecast
     山东夏季降水与前期热带洋区OLR的关系及其预测
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  tropical ocean area
Calculations by 1998 SCSMEX and TIPEX boundary layer data indicate that even in the lowest levels, eddy viscosity in the Tibetan Plateauan can be 2.3 times than in the tropical ocean area.
      
(4) The vertical structure of turbulence friction is quite different in the Plateau and in the tropical ocean area.
      
The results show that for this tropical ocean area the drag coefficientCD is equal to (1.53 ± 0.25) × 10-3 and the daily mean latent fluxHL is greater than its daily mean sensible fluxHs by a factor of about 9.
      
This paper describes results of the fluxes of momentum , sensible heat and latent heat for the West Pacific Tropical Ocean Area (127°E-150°E, 5°N-3°S).
      
In contrast to the point estimates produced by gauges, the radar estimates from KWAJ are true area averages for a tropical ocean area.
      


In this paper, results of the fluxes of momentum, sensible heat and latent heat for the West Pacific Tropical Ocean Area (from 127°E to 150°E, 5°N to 3° S) are described. The data were collected by the small tethered balloon sounding system over this ocean area including 6 continues stations from 11th of Octorber 1986 to the 15th of December 1986. These fluxes were calculated by the semiempirical flux-profile relationships of Monin-Obukhov similarity theory using these observed data. The results show that for...

In this paper, results of the fluxes of momentum, sensible heat and latent heat for the West Pacific Tropical Ocean Area (from 127°E to 150°E, 5°N to 3° S) are described. The data were collected by the small tethered balloon sounding system over this ocean area including 6 continues stations from 11th of Octorber 1986 to the 15th of December 1986. These fluxes were calculated by the semiempirical flux-profile relationships of Monin-Obukhov similarity theory using these observed data. The results show that for this tropical ocean area the drag coefficient CD is equal to (1.53±0.25) × 10-3, and the daily mean latent flux HL is greater than its daily mean sensible flux Hs, by factor of about 9.

本文根据中国科学院“实验3号”科学考察船1986年10月至12月在菲律宾以东60多万平方公里辽阔的西太平洋热带海域6个连续测站上(146°E,0°;145°E,0°;150°E,0°;140°E,5°N;145°E,5°N;150°E,5°N),使用我国自行研制的小型系留气艇探测系统观测到的大气温度、湿度、气压和风等廓线资料,利用相似理论的通量-廓线关系,给出这一海域的动量通量(特别是曳力系数C_D)、感热通量和潜热通量。结果表明,这一海域上的曳力系数值C_D=(1.53±0.25)×10~(-3);该海域总是将其贮存的热量以感热形式特别是以潜热形式输送到大气中(其中感热输送仅占10%,其余主要为水汽潜热输送),使该海域成为地球上不可多见的热源。

This paper describes the results of observation on the fluxes of momentum and sensible heat over Mizuho Station (70°41' 53 " S, 44°19 ' 54 " E), East Antarctica. The data were collected by using the meteorological tower 32m high at this station in 1979-1981 period. These fluxes were evaluated by semiemperical flux-profile relation of Monin-Obukhov similarity theory from these observed data, and the calculated result was compared with that over the West Pacific Tropical Ocean area and Beijing area....

This paper describes the results of observation on the fluxes of momentum and sensible heat over Mizuho Station (70°41' 53 " S, 44°19 ' 54 " E), East Antarctica. The data were collected by using the meteorological tower 32m high at this station in 1979-1981 period. These fluxes were evaluated by semiemperical flux-profile relation of Monin-Obukhov similarity theory from these observed data, and the calculated result was compared with that over the West Pacific Tropical Ocean area and Beijing area.

本文根据南极瑞穗站气温、风等平均廓线资料,利用相似理论通量一廓线关系计算得出了该站的湍流通量,并与西太平洋热带海域和北京地区湍流通量计算结果进行了比较。

According to the requirement of the International Satellite Cloud Climate Project(ISCCP ),a cloud parameters retrieval algorithm is designed,which is fit to derivecloudiness over East Asia and the Tropical Ocean area. The satellite data is obtainedfrom original S.VISSR of GMS-4,ranging from 50°N-30°Sand 80°-175°E,andcovering the midseason months──January,April, July and October of 1991. The totalmonthly mean cloudiness and hourly mean cloudiness are calculated with the methodmentioned above.The results...

According to the requirement of the International Satellite Cloud Climate Project(ISCCP ),a cloud parameters retrieval algorithm is designed,which is fit to derivecloudiness over East Asia and the Tropical Ocean area. The satellite data is obtainedfrom original S.VISSR of GMS-4,ranging from 50°N-30°Sand 80°-175°E,andcovering the midseason months──January,April, July and October of 1991. The totalmonthly mean cloudiness and hourly mean cloudiness are calculated with the methodmentioned above.The results are examined by comparing with OLR climatologieal datain the periods.Furthermore,not only the seasonal variations in cloudiness,such asmonsoon surge cloud system and the latitudinal movement of the ITCZ, but alsoseasonal distribution and the diurnal variability of cloudiness are studied in the region byusing the results.

参考国际卫星云气候计划和目前出现的几种云参数处理方法 ̄([1][2]),设计了一种适用于东亚和热带海洋地区的云参数处理方法,并着重进行了总云量的反演.处理的资料取自GMS-4的S·VISSR资料 ̄[3],覆盖范围为50°N-30°S,80°-175°E.时间为1991年的1、4、7、10四个月.使用上述方法对卫星资料计算得到了日、旬、月的平均云量,通过与其它资料和处理结果的对比分析,对处理方法和处理结果的真实性进行了初步检验。利用1991年4个典型月份的处理结果,研究了大范围云的季节变化,如赤道辐合带云系和副热带高压少云区的纬向移动,季风云系的爆发等;研究了一些局地区域云的季节分布;并对处理区域内云量的日变化进行了研究.

 
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