sensible heating中文是什么意思

• 等湿加热

• sensible    adj. 1.能感觉到的；可觉察的；明显的。 2.发觉； ...
• heating    adj. 1.加热的；供热的。 2.刺激的。 ...
• be sensible    通达事理
• be sensible of    意识到…
• sensible    adj. 1.能感觉到的；可觉察的；明显的。 2.发觉；觉悟；明白；感知；知道 (of). 3. 懂事的；有常识的；通情达理的；明智的；合情合理的；有理智的；(人、方法等)聪明的。 4.有知觉的。 5.(计划等)切合实际的；实用的。 6.(数量等)相当大的。 7.〔古语〕易感的；敏感的 (to)。 a sensible change for the better [worse] 显著变好[坏]。 He was sensible enough to mind his own business. 他很聪明，不管别人闲事。 I'm very sensible of your kindness. 我深感您的好意。 sensible clothing 实用的衣服。 a sensible idea 明智的意见。 a sensible man 聪明人。 a sensible plan 切合实际的计划。 a sensible proposal 合理的建议。 a sensible reduction in price 大幅度降价。 n. -ness 懂事；明智。
• sensible of    见到害羞; 觉查到
• to be sensible    本句与
• a sensible child    懂事的孩子
• a sensible point    叫它做一个觉点
• a sensible suggestion    明智的抉择
• machine sensible    机粕读的; 机器感知的
• machine-sensible    机器可读的
• sensible appearance    可感觉现象
• sensible atmosphere    可感大气; 阻尼大气
• sensible cooling    等湿冷却
• sensible earthquake    有感地震
• sensible enthalpy    敏感焓; 显焓
• sensible entropy    显熵
• sensible factor    敏感因素
• sensible form    感知形式
• sensible heat    【物理学】显热 (opp. latent heat)。
• sensible horizon    测者真地平; 感觉地平圈; 视地平圈; 视水平面
• sensible perspiration    可感觉出汗; 可感蒸发; 显汗; 知觉发汗
• sensible phenomenon    感觉得到的现象 感觉得到的现象
• sensible plan    切合实际的计划

• Based on the importance of heat flux variability to the earth ' s climate change and the dependence of the study about heat flux variability on the accuracy of heat flux data , this study will focus on the quality evaluation of heat flux datasets available and seasonal and interannual variability of latent and sensible heat fluxes in the tropical atlantic ocean
  基于海表潜热和感热通量的时空变化在全球变化中的重要性和海表潜热和感热通量研究对热通量资料产品精度的依赖性，本文重点就现有热通量资料产品的质量和热带大西洋海表潜热和感热通量的季节和年际变化开展较深入的研究。
• The characteristic of surface radiation , energy balance , albedo , bulk momentum transfer coefficient cd and bulk sensible heat transfer coefficient ch between surface and atmosphere over rainfed field are analyzed based on the data of land - surface process field experiment in the dingxi arid meteorology and ecological environment experimental station
  利用中国气象局兰州干旱气象研究所定西干旱气象与生态环境试验基地取得的地气相互作用观测试验资料，分析了地表辐射、地表能量平衡、地表反射率、总体输送系数等特征。
• 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。
• The maximum of instantaneous global radiation is beyond 1000w / m2 and the ten - days average intensity is 338 . 90w / m2 because of high atmospheric transparency over semi - arid rainfed agriculture region of loess plateau between june and august . global radiation , reflected global radiation and surface long wave radiation emerge the characteristic of daily variations on a typical clear day and cloudy day , whereas atmospheric long wave radiation has not this characteristic . meanwhile , net radiation , latent heat flux sensible heat flux and soil heat flux appear the same characteristic as the mean daily variations above spring wheat field and bare soil on a typical clear day and cloudy day
  黄土高原半干旱雨养农业区夏秋季大气透明度较高，晴天地面的总辐射值最大瞬时值均超过1000w m ~ 2 ， 6 8月总辐射旬平均强度为338 . 90w m ~ 2 ；典型晴天和阴天总辐射、反射辐射、地表长波辐射均表现出明显的日变化特征，而雨天没有明显的日循环规律；无论是晴天、阴天还是雨天，大气长波辐射基本没有明显的日变化规律。
• 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) 。
• 6 ) the correlation relationships of the mjo of daily 10m - wind ( v ) fields with that of sst fields are investigated by time - lagged svd method in the north pacific , south pacific and the tropical eastern pacific , and the basal process of v and sst mjo obtained in the three areas , which is a negative feedback process drived by drift and sensible heat under the conditions of shallow mld , is probably the maintaining mechanism
  6 )用时滞svd方法分析了北太平洋、南太平洋、热带东太平洋区域10米高处逐日风(夕)场与sst场季内振荡的相关联系，得到了三区夕、 sst场季内振荡的基本过程，它们是由漂流和感热输送推动的一个负反馈过程，它以薄mld为存在条件，可能是sst季内振荡的维持机制。
• A very much different fluxes model was suggested for remote sensing estimation , which takes account of the effects of advections in vertically or horizontally anisothermal vegetations . the inter - exchange of heat can result in lower total sensible heat flux and higher total latent heat flux of the considered areas . this method is designed technically for the simulations of pixel , is a try of new generation effluxes model
  针对遥感基于像元计算的特点，提出一种全新的通量计算方法，模型的结构和思路专为遥感像元面上计算的特点而设计，主要考虑由地表非均匀和不连续性引起的像元内部热量交换? ?局地微平流对显热和潜热通量的影响，验证表明，这种考虑平流的非均匀模型可以较好地模拟地表非均匀状态下的热量通量。