And then , a example is given about calculating regional average water mass and thermal flux exchanges at land - atmosphere interactions in yangtze river lower by a statistical - dynamical approach through combining remote sensing data with ground measurement data 从野外观测事实的基础上讨论下垫面非均匀性对地表水热通量的影响；然后以长江三角洲为例，将遥感观测资料和常规资料结合起来计算区域平均水热通量。
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 order to study the variation characteristics of heat flux at nansha and xisha islands in the south china sea , the observational data from the ocean stations are calculated to obtain air - sea heat exchanges and the annual circulation of heat budget around the summer monsoon onset in 1998 摘要为探索西沙和南沙海气热通量时间演变特征，用海洋站观测资料计算了1998年南海夏季风爆发前后，海气界面热量交换值及海面热收支年循环。
( 3 ) for parameterization of the sensible heat , the positively correlation between surface temperature and bulk transfer coefficient lead to a positive additional sub - scale flux . its magnitude is determined by the grid average roughness and average wind velocity on the reference level ( 3 )对区域感热通量的计算而言，由于地表温度和整体输送系数产生一个正的次网格通量项，它主要由网格平均粗糙度和参考高度平均风速所决定。
Net radiation absorbed by ice surface only account for 6 of that absorbed by the sea surface and it is consumed mainly by the processes of sensible heat exchange and ice melting , deficit part of the heat is compensated from the latent heat released when water vapor is frozen on ice surface and heat stored in ice 冰面吸收的净辐射仅为海面的6左右，主要消耗于感热输送和冰面融化过程，不足部分由水汽在冰面上凝结释放的潜热和冰中的热通量来补充。
In this paper , we have studied the transmission of a plane wave through a 1d quasiperiodic or aperiodic chain by numerical method . moreover the heat conduction for these chains is calculated . it is found that the heat flux j ~ n - 1 ( 0 . 5 < < 1 ) , and depends on the on - site potentials 本文首先用数值方法，计算了各种频率的平面波通过以上几种典型的一维准周期和非周期链的透射系数，并据此研究了这几种一维准周期和非周期链的热通量j与粒子数n之间的关系，得出j n ~ ( a - 1 ) ， 0 . 5 1 ，与系统中在位势的大小有关，并与其他系统的结果作了比较。
A three - dimension baroclinic prognostic model on the o - coordinate is established based on pom to simulate the wintertime circulation and the eddies in the east china seas , considering the topography , inflow and outflow on the open boundary , yangtse runoff , heat flux and wind stress on the sea surface 本文在pom模式基础上，建立一个坐标系下的三维斜压预报模式，考虑了海底地形、外来流、长江径流、海面风应力、海面热通量等多方面因素的影响，模拟结果较好地体现了冬季东中国海环流及涡旋的特征。
By theoretical analysis and experimental investigation to the exasperate position of the heat transfer in the umbrella - plate falling film evaporator , the exasperate experimental formula of the heat transfer was obtained . with the same reynolds , the high - point heat flux density of umbrella - plate evaporator is higher than vertical - plate evaporator could be observed from above formula , which maked out that with little reynolds liquid film was not easy to break 在实验条件下得出了伞板式降膜蒸发器小流量下液膜破裂的实验关联式，此关联式表明极限热通量随临界雷诺数增大而增大，在相同的临界雷诺数下，伞板蒸发器的极限热通量大于直板形蒸发器的极限热通量。
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。
