warm air mass [′wȯrm ¦er ′mas] (meteorology) An air mass that is warmer than the surrounding air; an implication that the air mass is warmer than the surface over which it is moving. McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-...
Why are the poles warm and the tropics cold, and compared to what? An equivalent question is: what determines the difference in temperature between tropics and poles, and can we understand why that difference has the magnitude it has on the real planet E
advection fog air conditioning air heating system Air Masses Air-Mass Modification Allen's rule Alma-Arasan Anapa angina Arctic Arctic Ocean Asia Atlantic Ocean Barents Sea bora Brooder calefaction climate cold boot References in periodicals archive ? Your body will warm up quickly and safely if it...
Hsu, S. A., 1984: Effect of cold-air advection on internal boundary- layer development over warm oceanic currents. Dyn. Atmos. Oceans, 8, 307-319.Hsu, S. A.: 1984, ‘Effect of Cold-Air Advection on Internal Boundary-Layer Development over Warm Oceanic Currents’, Dyn. Atmos. Oceans ...
The occurrence of cold days and cold spells was particularly related to the advection of air masses from the north-western sector. The occurrence of warm days and warm spells was related to the advection of air masses from the south-west.Polish Polar ResearchTOMCZYK, Arka...
PURPOSE: the wind that a kind of cold and heat air system can automatically control direction and intensity is provided to change the system in the case where, by comparing the position of body temperature information and user, to obtain data. ;CONSTITUTION: a kind of cold and heat air syst...
1)south-deflected warm&moist airflow偏南暖湿气流 2)warm and wet flow暖湿气流 1.The results show that the warm and wet flow on the edge of subtropical high and the high-level westerly trough supply the better large-scale circulation background for the rainstorm.利用高空、地面观测资料及多普勒...
Temporal changes in atmospheric conditions such as sea surface winds, surface air temperature, and surface air humidity cause upper ocean variability by modulating momentum and heat exchanges between the atmosphere and ocean. In the North Pacific, atmospheric fields differ greatly between the cold and ...
2) cold-worm air 冷暖空气3) Cold and warm air 冷暖气团4) Cold(Warm)advection 冷(暖)平流5) warm and wet flow 暖湿气流 1. The results show that the warm and wet flow on the edge of subtropical high and the high-level westerly trough supply the better large-scale circulation ...
1) Cold(Warm)advection 冷(暖)平流 2) the cold air and warm air current 冷暖气流 3) warm advection 暖平流 1. The measos cale systems of the east low- level jet and warm advection,and velocity field a re obvious signals for forecasting heavy r. 利用新疆阿克苏CINRAD/CC多普勒天气雷达...