A hugh human body of wait that has actually the same temperature, humidity, and air press at any type of given height; A solitary air mass might spread over millions of square km and be up to to 10 kilometres deep.

You are watching: How do scientists classify air masses

f1) type north of 50 degrees N latitude and south 50 levels S latitude, and2) have actually have high waiting pressure
1. Marine air masses: kind over oceans/ water evaoporates indigenous oceans, therefore the air can become really humid2)Continental wait masses: form over land; have less exposure to large amounts of moisture from bodies of H2O.; ergo, are an ext drier than naval air masses
1. Warmth humid waiting masses type over dry oceans.2. Maritime tropical wait masses that type over the Gulf that Mexico and the Atlantic s move 1st toward SE US.3. Castle then move N and NE, wherein they influence weather in the main and east US.4. In the west, maritme tropical air masses type over the Pacific Ocean and mainly affect weather on the West Coast; as they cross the coastal mountain ranges, the Pacific wait masses lose moisture.5. In summer, maritime tropical aire masses usually carry hot, humid weather.6. Plenty of summer showers and also thunderstorms in the eastern US develop in waiting masses the have developed over the Gulf of Mexico;7. In winter, humid wait mass can lug heavy rain or snow.
1. Cool, humid wait masses from over icy cold N. Pacific and N. Atlantic oceans2. Marine polar wait massesd influence the west coast mor climate the east Coast3. Also in summer, these masses the cool, humid air often carry fog, rain,a nd cool temperatures to the West Coast




See more: 2004 Hyundai Santa Fe 2.4 Timing Marks, 2004 Santafe 2