IPA

CLOUD FORMATION
STEAM ATMOSPHERE WATER CONTENT <2% OF TOTAL VOL ATMOSPHERE.
STEAM WATER CONTENT MAY VARY BETWEEN 0% - 3% IN
LINTANG REGIONAL SECONDARY & BE IN THE REGION 4% wet tropical.

TEMPERATURE IN THE ATMOSPHERE, AIR COMPONENT IS satu2nya
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:

Is the circulation of water from the oceans TO KEEP STARTING TO AIR
AND BACK TO SEA

Processes that occur in the hydrological cycle, INCLUDE:
Evaporation, condensation, precipitation, transpiration, MOVEMENT
MASS AIR & GROUND WATER MOVEMENT

Evapotranspiration: Evaporation of water through evaporation DIRECT
And transpiration through the leaves of plants COLLECTIVELY

WILDERNESS AREA, BUT INADEQUATE moisture LESS ENERGY,
Evaporation always occurs ANY TIME WHEN AVAILABLE BUT WATER
Precipitation so sparse that the hydrological cycle BE
PASSIVE
ON A BELT LINTANG, evaporation> DP BULK RAIN.
While at latitudes OTHERS, BULK RAIN> DP evaporation
TO ACHIEVE BALANCE, there should TRANSFER AIR /
STEAM WATER (& ALSO ENERGY)