迎风

基本解释 (translations)

aweather

词组短语

on the wind · facing the wind · against the wind · with the wind

与迎风相关的网络例句 [注：此内容来源于网络，仅供参考]

Be the construction aweather with the width of the beam wind along high press consecution regulation the variety, table 7 inside of pulsation influence coefficient again multiply by with the correction coefficient ob with ov.

2，当结构迎风面和侧风面的宽度沿高度按连续规律变化时，表7中的脉动影响系数再乘以修正系数ob和ov.0b应为构筑迎风面在z高度处的宽度bz与底部宽度bo的比值，ov可按表7确定。

Automotive frontal area is projected area of automobile driving direction,which is necessary parameter of measuring automotive air drag coefficient.

汽车迎风面积是指汽车在行驶方向的投影面积，汽车迎风面积是求汽车空气阻力系数的必需参数。

Distinctive pale leaf undersides, giving fluttery appearance in a strong breeze, hence "turn-in-the-wind".

下面清晰的苍白的叶，在迎风飘扬时赏心悦目，由是得英文名 'turn-in-the-wind' 迎风而变

The south and north of the windward side of the Annam Cordillera show great difference in the diurnal variation of rainfall, which is related to migration of rainfall. Rainfall over coastal areas of the Thailand Gulf in 01-04LST migrates to inland northeastwards and then heavy rainfall occurs over areas southwest of the Annam Cordillera in 16-19LST, after that heavy rainfall migrates northwestward along the Annam Cordillera to areas northwest of the Annam Cordillera in 01-04LST in the next day. The migration of rainfall results in different characteristics of diurnal variation on the windward side of Annam Cordillera.

长山山脉西侧迎风坡的一南一北两个区域，表现出明显不同的降水日变化特征，其原因与降水的传播有关。01-04LST，降水大值区出现在泰国湾东部沿海，并向中南半岛岛内传播，16-19LST在长山山脉西南侧形成降水大值区，之后降水进一步沿山脉向西北传播，并于次日01-04LST传到长山山脉西北侧区域，通过降水的这种传播特征从而导致长山山脉迎风坡一侧不同的降水日变化特征。

The resulting upwind-performance gets you further upwind and does it much faster than ever before.

收效的迎风表现得到您进一步迎风和快速地做它。

The results show that, for the first with no headwall, when there is no crosswind, it has small front face areas, so the aerodynamic resistance is the least. Since the second and the third have headwall, the front face areas are large, so they have bigger aerodynamic resistance. Under the condition of crosswind, as the third design option has the highest side beam, the area of positive pressure at the upwind is bigger, and the area of negative pressure is smaller when the bigger eddy area appears, so the side forces become larger. The first has the least side forces; the overturning moment of the first is the least.

研究结果表明：在无横风情况下，方案一中没有端墙，迎风面积较小，受到的气动阻力最小，方案二和三中平车有端墙，迎风面积较大，受到的气动阻力也较大；有横风情况下，方案三中平车侧梁较高，车体迎风面正压区较大，而背风侧产生较大的涡流区，在此区域内压力较小，故其横向力较大，方案一中平车侧梁没有加高，受到的横向力最小；方案一中平车倾覆力矩最小，稳定性最好。

The results showed that the flow reattachment distance in the lee side of various dune models are ranged from 4.8H to 10.8H depending on different stoss slopes, the maximum of flow reattachment distance was found in the lee side of the transverse dune with a 15° stoss slope angle.

实验结果表明，当来流风速垂直于沙丘脊线时，沙丘背风侧的气流重附距离介于4.8H～10.8H之间，最大重附距离出现在迎风坡坡度为15 的沙丘背风侧；沙丘迎风坡坡度是控制背风侧气流重附距离的主要因素，而自由风速对气流重附距离的控制作用较小。

The field experiments on the near surface airflow, sand transport rate, grain size of the dune sands and the morphology of the dunes show that though shear velocity decreased at the toe of the transverse dune, the threshold shear velocity decreased simultaneously. The decreased threshold shear velocity and unsaturated sand flows at the stoss slope of the dunes resulted the erosion at the toe of the dune.

对简单横向沙丘表面的气流、输沙率、物质结构，以及形态学特征的观测表明，在横向沙丘迎风坡坡脚尽管剪切速度有所下降，但起动剪切速度同时减小，起动剪切速度减小与不饱和风沙流是沙物质在迎风坡坡脚不能产生沉积的主要原因。

Field measurement of surface wind velocity and sediment transport rates was made on barchan dune in Wulanbuhe desert to understand. The results show that the wind velocities increasing upon windward slopes of the dunes vary with both slope morphology and wind velocity at the foot of the dunes.

对乌兰布和沙漠新月形沙丘表面风速的野外观测结果表明，沙丘迎风坡气流加速量主要和沙丘坡面形态、迎风坡前来流风速有关，迎风坡风速放大率介于1.02~1.59之间。

The density of the foot 、middle part and top are 124grain /m~2、91 grain /m~2、66 grain /m~2,the seeds is more little windward than the leeward.The density of seed banks in windward is 81grain/m~2 and the leeward density is 100grain/m~2.The seed of ephemerals bourgeoning reaches the pinnacle on April and May.The diversity of different parts sand dune is different,but the differences do not reach the marked level.The similarity is high between the seed banks and the vegetation.

迎风坡种子库密度比背风坡面少，迎风坡种子库平均密度为81粒/m2，而背风坡种子库平均密度为100粒/m2；短命植物种子在4月上旬达到萌发高峰，沙丘不同部位物种多样性存在差异，土壤种子库和地上植被存在较高的相似性，此外短命植物在沙丘不同部位的分布存在较高的空间异质性。

与迎风相关的网络解释 [注：此内容来源于网络，仅供参考]

close-hauled：迎风航驶

close harbor 有闸港池 | close hauled 迎风航驶 | close ice 密集冰

close-hauled：紧航 近迎风

Race 航次 轮 | Close-hauled 紧航 近迎风 | Moving Astern 倒退行驶 向後运动

close-hauled：迎风航行

724 紧密配合 close fit | 725 迎风航行 close-hauled | 726 紧密铆[接] close riveting

on a lee shore：船在下风岸(即迎风岸

on a lay 船长包船拆帐制 | on a lee shore 船在下风岸(即迎风岸 | on a wind 迎风航驶

on the wind：迎风航驶

on the weather beam 在上风正横方向 | on the wind 迎风航驶 | on the wind 迎风航驶迎风航驶

on the wind：迎风航驶迎风航驶

on the wind 迎风航驶 | on the wind 迎风航驶迎风航驶 | on the wrong tack 航向错误

bring up to the wind：将船迎风停住

bring up to the wind 将船迎风停止 | bring up to the wind 将船迎风停住 | bring up with a round turn 急速拉住正松出的缆绳

bring up to the wind：将船迎风停止

bring up anchor 抓住海底的锚 | bring up to the wind 将船迎风停止 | bring up to the wind 将船迎风停住

windward slope：迎风坡

暖湿气流遇到山地,沿坡上升,水汽凝结,兴云降雨;故迎风坡(windward slope)的雨量随高度增加而递增,但山地很高时,超过某一高度後,又逐渐减少. 盛行东北季风期间,台湾东北部位在雪山山脉和中央山脉的迎风坡,多地形雨;西南部位在背风坡,

windward side：迎风边

windward anchor 顶风锚 | windward side 迎风边 | windward slope 迎风坡