CLOUD FORMATION

CLOUD FORMATION 

STEAM ATMOSPHERE WATER CONTENT <2% OF TOTAL VOLUME ATMOSPHERE. STEAM WATER CONTENT MAY VARY BETWEEN 0% - 3% IN THE MEDIUM & CAN LINTANG 4% in the tropics WET. TEMPERATURE IN THE ATMOSPHERE, THE AIR IS HIS ONE COMPONENT YG ATMOSPHERE TO FORM 3 FORM OF EXPOSURE: CAIR (AIR), GAS (UAP), OR SOLID (ES). CHANGES FROM ONE FORM TO ANOTHER FORM D IN NATURE OCCUR IN A CYCLE D IN CALL hydrology Hydrological cycle REQUIRE HEAT ENERGY & humidity ENOUGH.

Hydrologic cycle:
AIR CIRCULATION IS THAT REMAINS FROM THE OCEAN TO THE AIR AND BACK TO SEA PROCESS WHICH OCCURRED ON hydrological cycle, INCLUDE: Evaporation, condensation, precipitation, transpiration, MOVEMENT MASS AIR AND GROUND WATER MOVEMENT Evapotranspiration: evaporation of water evaporation DIRECT And transpiration LEAVES BY MUTUAL TUMBUH2AN WILDERNESS AREA, BUT INADEQUATE moisture LESS ENERGY, Evaporation ALWAYS HAPPENS WHEN WATER AVAILABLE AT ANY TIME BUT Precipitation VERY RARELY BE SO hydrologic cycle PASSIVE ON A BELT LINTANG, evaporation> DP BULK RAIN. While on LINTANG THE OTHER BULK RAIN> DP evaporation TO ACHIEVE BALANCE, HAVE NO WATER TRANSFER / STEAM WATER (AND ALSO ENERGY)