潜热通量的英文

• latent heat flux

• "潜热"英文翻译    latent heat
• "通量"英文翻译    flux; shower
• "海面蒸发潜热通量" 英文翻译 :    latent flux of sea surface evaporated
• "热通量" 英文翻译 :    heat flux; thermal flux; thermoflux; tone'smal flux
• "壁间热通量" 英文翻译 :    wall heat flux
• "壁面热通量" 英文翻译 :    wall heat flux
• "层流热通量" 英文翻译 :    laminar heat flux
• "低热通量" 英文翻译 :    low heat fluxes
• "峰值热通量" 英文翻译 :    peak heat flux
• "高热通量" 英文翻译 :    high-heat flux
• "局部热通量" 英文翻译 :    local heat flux
• "临界热通量" 英文翻译 :    critical heat flux
• "热流热通量" 英文翻译 :    heat flow
• "热通量矢量" 英文翻译 :    thermal flux vector
• "热通量向量" 英文翻译 :    heat flux vector
• "热通量仪" 英文翻译 :    fluxplate
• "烧毁热通量" 英文翻译 :    burn-out flux; burn-out heat flux
• "瞬时热通量" 英文翻译 :    transient heat flux
• "土壤热通量" 英文翻译 :    soil-heat flux
• "轴向热通量" 英文翻译 :    axial heat flux
• "总热通量" 英文翻译 :    total heat flux
• "最大热通量" 英文翻译 :    maximum heat flux
• "临界热通量比" 英文翻译 :    critical heat flux ratio
• "热通量变换器" 英文翻译 :    thermal flux transformer
• "热通量浓度比" 英文翻译 :    thermal flux concentration ratio

• The half - year cycle of latent heat flux exists in the xisha area , with the maximum appearing in winter
  西沙海面潜热通量存在半年周期特征，极大值也是出现在冬半年。
• There are negative latent and sensible heat fluxes in south and east of the cyclone central area after it moved to ocean
  气旋出海后在气旋中心区南方和东方存在负潜热通量和感热通量区。
• The distribution and variation of latent and sensible heat fluxes of the cyclones were discussed based on the numerical simulation
  在数值模拟基础上重点讨论了出海气旋发展过程潜热通量和感热通量的分布及其演变情况。
• In equatorial regions , the air - sea humidity difference is overestimated in whoi relative to pirata , which leads to the biases in latent heat flux
  在赤道区， whoi对海气湿度差的估计相对于pirata偏高，直接导致其对潜热通量的估计偏差。
• ( 2 ) based on gaining the surface parameters , to compare to diversified retrieve model to choose optimal one to retrieve net radiance flux , soil heat flux and latent heat flux , which settle the groundwork to calculate the regional et
  在获取地表参数的基础上，反复对比前人各种遥感反演模型，选择最佳模型对长江三角洲的区域净辐射通量、土壤热通量、潜热通量进行了反演，为计算区域蒸散量奠定了基础。
• Especially , global transformation , the water balance , carbon balance and drought forecast in district , etc , which all require quantitative surface flux . by all appearances , these fluxes all do n ' t need to be distributed in spots , but in area
  尤其全球变化、区域水分平衡、碳平衡和区域旱灾预报等等都需要定量的地表通量信息(辐射通量、显热通量、潜热通量、土壤热通量) 。显然，这些通量均要求区域分布的而不是单点数据。
• In the region north of brazil , although both wind speed and air - sea humidity difference have dramatic variations , the variation of latent heat flux is just ordinary in magnitude . the reason is that the variations of wind speed and air - sea humidity difference are out of phase with each other so that they decrease each other greatly
  在巴西以北的暖水区，尽管海气湿度差的变化和风速的变化都较大，但二者在区域内总是反相，彼此削弱了对潜热通量变化的贡献，所以该区潜热通量的变化振幅较小，最终由风速的变化主导潜热通量的变化。
• The results show that the local average temperature and average surface temperature will rise , and both daily difference will rise , too . average sensible heat flux and its daily difference will also increase while average latent heat flux and its daily difference will reduce after the vegetation degration of some area in the west of liaoning province ; the average temperature will raise 0 - 0 . 5 , average surface temperature will raise 0 - 1 . 0 , average sensible heat flux will increase 5 - 40w / m2 , about 8 - 55 % and average latent heat flux will reduce 5 - 60w / m2 , about 4 - 48 %
  模拟结果表明：在辽西部分地区植被退化后，当地6 、 7 、 8三个月的夏季平均气温和平均地面温度升高，两者的日较差增大，平均感热通量及其日较差也增大，平均潜热通量及其日较差减小；平均气温升高0 0 . 5 ，平均地面温度升高0 1 . 0 ，平均感热通量增大5 40w / m ~ 2 ，约8 55 ，平均潜热通量减小5 60w / m ~ 2 ，约4 48 。
• In equatorial region , the mean air - sea humidity difference is much smaller , so the variations of air - sea humidity difference under large mean wind speed dominate the variations of latent heat flux . the ocean release the most heat during the period from march to may , when sst is highest in the whole year because sst dominates the variation of air - sea humidity difference
  在赤道冷舌区，平均的背景海气湿度差比较小，所以平均风速背景下的海气湿度差的热带大西洋海表潜热和感热通量的季节和年际变化研究变化主导该区的潜热通量的变化。
• In short , through retrieving the parameter such as surface albedo , surface temperature and surface emissivity , all the energy flux such as net radiance flux , soil heat flux and latent heat flux can be computed in sequence further , then latent heat flux which provide energy for et can be computed based on energy balance equation , finally instantaneous et and daily et can be obtained
  总之，根据地表能量平衡方程，通过计算对地表反照率、地表温度、地表比辐射系数、归一化植被指数等参数进行反演，进一步计算出了地表净辐射通量，土壤热通量和潜热通量，最后获得了遥感影像成像时的瞬时蒸散及当天的总蒸散量。