土壤热通量的英文

• soil-heat flux

• "土壤"英文翻译    soil; ground; pedogenesis; p ...
• "通量"英文翻译    flux; shower
• "土壤热" 英文翻译 :    soil heat; soil thermal
• "热通量" 英文翻译 :    heat flux; thermal flux; thermoflux; tone'smal flux
• "土壤热传导" 英文翻译 :    soil heat conduction soil thermal conduction
• "土壤热交换" 英文翻译 :    soil heat exchange soil thermal exchange
• "土壤热流" 英文翻译 :    soil heat flow
• "土壤热平衡" 英文翻译 :    soil heat balance soil thermal balance
• "土壤热容量" 英文翻译 :    soil heat capacity soil thermal capacity
• "土壤热特性" 英文翻译 :    soil thermal characteristic
• "土壤热源" 英文翻译 :    soil heat source
• "土壤热状况" 英文翻译 :    soil heat regime soil thermal regime
• "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
• "潜热通量" 英文翻译 :    latent 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

• Moreover , evapotranspiration consumes mainly net radiation on a clear day and sensible heat flux is greater than latent heat flux on a cloudy day above spring wheat field
  在有植被覆盖或裸地下垫面，晴天、阴天的净辐射、潜热、感热及土壤热通量均表现出了与平均状况一样的日变化特征。
• ( 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 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。
• Soil heat flux from atmosphere to soil is about 5 % of net radiation on a clear and cloudy day and soil discharge energy to atmosphere on a rainy day above the same field . in brief , average latent heat , sensible heat and soil heat flux is 40 % . 50 % and 10 % of net radiation respectively
  在春小麦下垫面，晴天能量主要消耗于农田蒸散，而在阴天显热交换大于农田蒸散耗热；在晴天和阴天大气向土壤的能量传输均维持在净辐射的5左右，雨天时，土壤热通量为负值。
• Some variables regional distribution over south ningxia is given out in the course of evapotranspiration estimation : the regional distribution of surface characteristic parameters ( normalzed difference vegetation index , surface albedo , surface temperature ) , radiation balance components ( surface absorbed shortwave radiation , surface longwave radiation , atmospheric counter radiation , net radiation ) , surface heat and balance components ( soil heat flux , sensible heat flux , latent heat flux )
  估算区域蒸发(散)量的过程中，得到许多有意义的量：地表特征参数(植被指数ndvi 、地表反射率、地表温度) ；地表辐射平衡各量(地表短波吸收辐射、地表长波辐射、大气逆辐射、地表净辐射) ；地表热量平衡各量(土壤热通量、显热通量、潜热通量) 。
• Similarly , the net radiation on a cloudy day is mainly used up evaporation of soil . the integrated value of soil heat flux is negative on a cloudy day and that shows the soil emits the heat , which is different on a clear day . in short , average latent , sensible and soil heat flux is 67 % , 21 % and 6 % of net radiation respectively
  在裸地下垫面时，晴天潜热占到净辐射的60 ，显热交换只占到19 ，在阴天净辐射同样主要消耗于土壤蒸发，与晴天不同的是在阴天土壤热通量积分值小于零，表明土壤在向外释放热量；平均状况下，潜热、显热和土壤热通分别占到净辐射的67 、 21和6 。