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Topic 8: Water and Climate

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Page 1: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Topic 8:Water and Climate

Page 2: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

The Water Cycle

• Climate – the conditions of the atmosphere over long periods of time

• Water cycle – the movement and phase changes at and near Earth’s surface Fueled by insolation and gravity Also known as the hydrologic cycle.

Page 3: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

The Water Cycle

• 97% of Earth’s water is held in oceans

• About 80% of Earth’s fresh water is in glaciers

• Graph of pg 160 in book

Page 4: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

The Water Cycle

• Four places that precipitation goes if it lands on land: Water retention: water is held on land as

ice or snow or on leaves of trees and plants

Infiltration: soaks into ground Runoff: flows over Earth’s surface Evapotranspiration: water evaporates,

sublimates or transpirates back into atmosphere Most precipitation returns to

atmosphere

Page 5: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Condensation and sublimation(cloud formation)

Precipitation

SublimationTranspiration

Runoff

Zone of aeration

Water table

Zone of saturation

Bedrock = impermeable

Evaporation

Infiltration

Page 6: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Factors Affecting Infiltration

• 7 Factors affecting infiltration: Slope of the land Degree of saturation Porosity Permeability Capillarity Vegetation Land use

Page 7: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Slope

• What effect does slope of the land have on infiltration Steeper slope = less infiltration

slope

Infilt

rati

on

Page 8: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Degree of Saturation

• What effect does degree of saturation have on infiltration?

The more saturated the ground = less infiltration

saturation

Infilt

rati

on

Page 9: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Vocabulary• Zone of aeration – pores of soil

partly filled with air and partly filled with water (capillary water)

• Zone of saturation – pores of soil are filled with water

• Water table – interface between zone of aeration and zone of saturation

• Groundwater – subsurface water below the water table

Page 10: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Porosity

• Porosity – percent of open pore space in a material compared to its total volume

• What effect does porosity have on infiltration? The greater the porosity the greater

the infiltration

Page 11: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Porosity

• Effect of the particle characteristics on porosity: Shape: round particles = high

porosity angular particles = low

porosity Packing: loose = high porosity

packed = low porosity Sorting: sorted = high porosity unsorted = low porosity Size: DOES NOT AFFECT POROSITY

Page 12: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Permeability

• Permeability – how easily water passes through a material Permeability rate – how fast water

passes through a material

• Two factors that affect permeability How well connected pores are Size of pores

Page 13: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Permeability

• What effect does permeability have on infiltration? The more permeable the ground is

the more water will infiltrate The more permeable the faster water

will infiltrate (less time)

Page 14: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Capillarity

• Capillarity – the “stickiness” of water to ground particles

• Why is capillary action important? It brings water to the roots of plants

• What is the effect of particle size on capillarity? Smaller particles = greater capillarity

= more capillary water

Page 15: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Vegitation

• What is the effect of vegetation on infiltration? More vegetation = more infiltration

less runoff Less vegetation = less infiltration

more runoff

Page 16: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Land Use

• What is the effect of land use on infiltration? Urbanization decreases infiltration

More paved surfaces (roads, parking lots, buildings)

More runoff

Page 17: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Runoff

• What are the situations that can lead to runoff? Rate of precipitation is greater than

rate of infiltration (permeability rate) Pore space if saturated Slope is too steep to allow infiltration Water on surface has not evaporated

Page 18: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Stream Discharge

• Stream discharge – the amount of water flowing past a spot in a certain amount of time m3/s or L/s

Page 19: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Flooding

• Flooding is the result of: When a stream overflows its channel When precipitation is greater than

infiltration A hurricane storm surge Rising sea Sinking land

Page 20: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Climate

Page 21: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Climate

• Climate – the conditions of the atmosphere over long periods of time

Page 22: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Temperature and Moisture

• Two important factors concerning temperature and climate: Average temperature throughout the

year Range of monthly average

temperatures

Page 23: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Evapotranspiration

• Potential evapotranspiration – amount of water that would evapotranspirate if water was available Determined by temperature

(available energy)

Page 24: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Arid Climates

• An arid (dry)climate occurs when total precipitation is less than potential evapotranspiration Atmosphere can evaporate more

water than is falling

Page 25: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Humid Climates

• A humid (moist) climate occurs when precipitation is more than potential evapotransipiration Atmosphere is trying to evaporate

less than is falling

Page 26: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Factors affecting Climate

• 8 Factors affecting climate Latitude Planetary wind and pressure belts Oceans and large bodies of water Mountains Elevation Cloud cover Vegetation

Page 27: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Latitude

• How are latitude and temperature related? Higher latitude = lower temperatures

(yearly)

Page 28: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Latitude and Moisture

• What causes moisture conditions to vary with latitude? Planetary wind and pressure belts

Lows = humid climates Highs = deserts, arid climates

Page 29: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Latitude and Moisture

• At what latitudes are there moist conditions? Why? 0o, 30 – 60o (mid latitudes) Low pressure – rising air cools =

precipitation

Page 30: Topic 8: Water and Climate. The Water Cycle Climate – the conditions of the atmosphere over long periods of time Water cycle – the movement and phase

Latitude and Moisture

• At what latitudes are there arid conditions? Why? Poles, 30oN, 30oS High pressure – sinking air

warms(compression) = lower RH