Hydrosphere

density of ocean water

depth of ocean water

evaporation of the ocean water

layering of ocean water

wind circulates heat in the air

heat from the core circulates ocean currents

ocean currents do not change temperatures

ocean currents circulate water from the equator

moving water from cold polar waters

moving water from warm equatorial waters

moving cold air to coastal regions

moving warm air up to the polar caps

removes heat from surface water and increases water density

removes heat from surface water and decrease water density

removes heat from deep currents and increases water density

removes heat from deep currents and decreases water density

air movement

density

turbidity

temperature increases

air

land

plants

water

moving water from aquifers to surface waters

moving deep current waters through the side of the water table

moving precipitation and surface water through the water table

human waste

water has over saturated the ground

light precipitation that lasts for an hour

low water levels

increased air circulation

groundwater accumulation

flooding

drought

hurricane

evaporation

evapotranspiration

infiltration

condensation