湿度差的英文

• hygrometric deficit
• psychrometric difference

• 湿度    humidity; dampness
• 差    send on an errand; dispatch
• 湿度    humidity; dampness 空气湿度 air humidity; 土壤湿度 soil moisture; 绝对[相对] 湿度 absolute [relative] humidity; 由于湿度高, 今晚屋子里不舒服。 the house is not comfortable tonight because of the high humidity.; 湿度变化 hygral change; 湿度表 hygroscope; hygrometer; humidometer; 湿度测量 humidity measurement; 湿度调节器[仪] humidistat; humidostat; 湿度图 hygrogram
• 幅度差    separation
• 高度差    altimeter lag; altitude difference; altitude differential; altitude intercept; diff h; difference in height; difference of altitude; elevation difference
• 黑度差    density differience
• 辉度差    luminance difference
• 角度差    angle difference
• 经度差    d lo; difference in longitude; difference of longitude; longitude difference
• 亮度差    luminance difference
• 流度差    mobility contrast
• 密度差    density contrast; density differences; difference in density
• 浓度差    concentration difference; concentration gradient; differential concentration
• 坡度差    difference in gradients
• 强度差    intensity difference
• 色度差    colour difference
• 深度差    depth differences
• 视度差    diopter difference
• 速度差    differential velocity; speed difference; speed differential; velocity contrast
• 纬度差    d lat; difference inlatitude; difference of latitude; tangent latitude error
• 温度差    difference in temperature; difference of temperature; hygrometric deficit; temperature approach; temperature contrast; temperature difference; temperature diverge; temperature head
• 潮湿度,润湿度    wetness
• height]高度差    diff h
• 北向纬度差    northing
• 边缘厚度差    edge thickness difference

• 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。
• It is found that the climatological mean of wind speed and air - sea humidity difference are both large , the variation of wind speed are almost in phase with air - sea humidity difference , yielding much larger or smaller latent heat flux . so the ocean release the most latent heat in its own winter of the two hemispheres when both wind speed and air - sea humidity difference are large
  发现在南北两信风区，风速和海气湿度差的变化几乎是同位相的，平均背景风速和海气湿度差都较大，他们互相加强彼此对潜热通量变化的贡献，所以海洋潜热损失最大是发生信风南北两区的各自风速和海气湿度差都较大的冬季。
• 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。
• 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 climatological itcz , the mean air - sea humidity difference is greater relatively so that the variation of wind speed under large mean air - sea humidity difference is the main factor influencing the variation of latent heat flux . the latent heat loss is greatest from june to august when the wind speed is largest in the region
  在气候平均的工tcz区，平均的背景海气湿度差比较大，所以平均海气湿度差背景下风速的变化主导潜热通量的变化，因此该区潜热损失最大值发生在风速最大的6一8月份。