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hydrological cycle 2.0
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The hydrologic cycle begins with the
evaporation
of water from the surface of the
ocean.
Moisture is transported around the globe until it returns to the surface as precipitation.
the most important are
evaporation
, transpiration,
condensation
, precipitation, and runoff.
By
evaporation
, water in the
liquid
state is transferred to the gaseous, or vapour, state.
Transpiration is the
evaporation
of water through
minute pores
, or stomata, in the leaves of plants.
The transition process from the vapour state to the liquid state is called
condensation.
By
condensation
, water vapour in the atmosphere is released to form
precipitation.
some may be intercepted by
vegetation
and then
evaporated
from the surface of leaves, some percolates into the soil by infiltration
the remainder flows directly as
surface runoff into the sea.