subtropical westerlies
- subtropical westerlies的基本解释
-
-
副热带西风带
- 更多网络例句与subtropical westerlies相关的网络例句 [注：此内容来源于网络，仅供参考]
-
It is found that in summer, the region between the southern edge of the westerlies and the northern margin in the subtropical anticyclone of the West Pacific is a favorable location for strong deep summer convection and MCS development.
夏季汛期降水主要受东亚夏季风的影响，非台风暴雨的出现与夏季风的进退一致。夏季在东亚西风带南缘和西太平洋副热带高压之间的地区，是夏季最有利于深对流和MCS发展的地区。
-
Lying in the North Hemispheric Subtropical High, the middle reaches of the Yangtze, as a key passage of the East Asian monsoon, is climatologically characterized by the energy exchange between the trade wind and westerlies as well as water-vapor convergence of the Southeast and Southwest monsoons.
长江中游地处北半球副热带，是东亚季风的必经之地。副热带附近东风与西风之间的能量交换和东南季风与西南季风的水汽辐合造就了该区环境的过渡带特征，使它灵敏地响应气候的变化。
-
As a result, a weak indirect cell is formed in high latitudes. By the 36th time step, the model atmosphere accomplishes the transition form one-cell circulation to two-cell circulation. There is a momentum source in the upper subtropical region. During the transition, the"polar westerlies jet"gets weakened and vanishes at the end, while the subtropical westerlies jet gets strengthened. At this two-cell stage, the generation and dissipation of westerly angular momentum do not balance each other, and the atmosphere is still at an unstable state with great surplus of angular momentum generation.
随着模式的运行，直接环流加强，地表东风带制造西风角动量加大，上支气流的加强，同样在科氏力的作用下，在副热带地区形成副热带西风急流，同时所谓的&极地西风激流&向赤道靠拢、减弱，最后消失，这时在整个半球形成了靠赤道的直接环流和靠极地一侧的间接环流，两圈环流形成的过程仅仅需要9个小时左右。
- 更多网络解释与subtropical westerlies相关的网络解释 [注：此内容来源于网络，仅供参考]
-
subtropical westerlies：亚热带午带
subtropical soil 亚热带土壤 | subtropical westerlies 亚热带午带 | subtropics 亚热带
-
subtropical westerlies：副热带西风[带]
"subtropical ridge","副热带[高压]脊" | "subtropical westerlies","副热带西风[带]" | "subtropical wind belt","副热带风带"
-
subtropical westerlies：副热带西风
副热带脊 subtropical ridge | 副热带西风 subtropical westerlies | 副热带风带 subtropical wind belt