等压面的英文

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"等压面"怎么读用"等压面"造句

英文翻译手机版

co tantpre uresurface
constant pressure surface
constant-pressure surface
isobaric surface
isobaricsurface
isopiestic level
isopiestic surface
isopressure surface
isostatic surface

"等压"英文翻译 isobaric
"面"英文翻译 face
"标准等压面" 英文翻译 : mandatory level; principal isobaric surfaces; standard isobaric surfaces; standardisobaricsurfaces
"等压面飞行" 英文翻译 : pressure-pattern flying
"等压面领航" 英文翻译 : aerolongation; pressure pattern navigation
"等压面坡度" 英文翻译 : isobaric slope
"等压面图" 英文翻译 : constant pressure chart; constant-pressure chart; isobaric chart; isobaric map
"等压面形势" 英文翻译 : pressure topography
"等压面图；等压线图" 英文翻译 : isobaric chart
"等压面高度图" 英文翻译 : constant-pressure altitude chart
"等压面环球送" 英文翻译 : transosonde
"等压面能量传送" 英文翻译 : isobaric energy transport
"非标准等压面图" 英文翻译 : nonstandard constant pressure chart
"等压" 英文翻译 : isobaric
"侧压面" 英文翻译 : side pressure surface
"测压面" 英文翻译 : piezometric surface; potential surface
"常压面" 英文翻译 : normal pressure surface
"承压面" 英文翻译 : bearing area; load bearing face; pressure bearing surface; pressure face; pressure surface; pressure-bearing surface
"冲压面" 英文翻译 : dieface
"低压面" 英文翻译 : low-pressure side
"定压面" 英文翻译 : constant pressure surface
"高压面" 英文翻译 : high pre ure surface; high pressure surface
"恒压面" 英文翻译 : constant pressure surface
"挤压面" 英文翻译 : extrude patch
"加压面" 英文翻译 : druckflche pressure surface

例句与用法

Terrain protrusion is shaded in grey in the chart
图中超出等压面的高地以灰色标示。
Standard isobaric surfaces
标准等压面
For " upper - air " , weather maps are usually drawn for isobaric ( i . e . equal pressure ) surfaces following the practice of conventional upper - air observations and analysis . air density and atmospheric pressure generally decrease as altitude increases
至于高空方面，由于常规的高空观测与大气分析都是在标准等气压面上进行，所以高空天气图亦习惯在等压面上绘制。
For the 60 - km orsm , the boundary conditions are prepared from jma s global spectral model outputs , which include surface data as well as upper level data on 16 standard pressure levels all the way up to 10 hpa about 30 km above ground in altitude
60公里外模式的边界条件，主要来自日本气象厅全球谱模式的输出数据，当中包括地面数据及16个标准等压面的高空数据，顶层在10百帕斯卡，即离地约30公里的高度。
In the atmosphere , geopotential varies with altitudes and across latitudes . on an isobaric surface , higher geopotential implies higher potential energy and vice versa . just like streams flow according to the layout of terrain , air will flow from high to low geopotential regions
在等压面天气图上，位势高的地方位能较高，位势低的地方位能较低，高空的气流会由前者流向后者，情况有点像河川根据山脊高低的分布而流动一样。
For the 60 - km orsm , the boundary conditions are prepared from jma s global spectral model ( gsm ) outputs , which include surface data as well as upper level data on 16 standard pressure levels all the way up to 10 hpa ( about 30 km above ground in altitude ) . boundary data for the inner 20 - km model are extracted from the outer 60 - km model
60公里外模式的边界条件，主要来自日本气象厅全球谱模式的输出数据，当中包括地面数据及16个标准等压面的高空数据，顶层在10百帕斯卡，即离地约30公里的高度。 20公里内模式的边界条件，则取自60公里外模式。