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GUID
ED
GR
AP
HIC
NOTES
68% OF EARTH S FRESH WATER IS FROZEN IN GLACIERS AND ICE CAPS.
A little over 30% OF EARTH S FRESH WATER IS GROUNDWATER . about .9% is Other surface water.(not Shown on
the graph).
LAKES AND RIVERS HOLD 89% OF OUR LIQUID SURFACE WATER.
97% OF EARTH S WATER IS SALT WATER IN THE OCEAN.
.001% OF EARTH S WATER IS IN THE ATMOSPHERE.
11% OF OUR LIQUID SURFACE WATER IS IN SWAMPS AND WETLANDS.
NAME CLASS
LAKES AND RIVERS HOLD 89% OF LAKES AND RIVERS HOLD 89% OF
3% of Earth s Water is fresh water.
Surface water is .3% of Earth s Water. That is 1/3 of 1%. all THE Lakes, Rivers, and swamps combined make that .3%.
97%
3%
68%
30%
.3%
89%
11%
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% OF EARTH S FRESH WATER IS FROZEN IN GLACIERS AND ICE CAPS.
A little over % OF EARTH S FRESH WATER IS Groundwater . about % is Other surface water.(not Shown on
the graph).
LAKES AND RIVERS HOLD % OF OUR LIQUID SURFACE WATER.
OF EARTH S WATER IS SALT WATER IN THE OCEAN.
% OF EARTH S WATER IS IN THE ATMOSPHERE.
% OF OUR LIQUID SURFACE WATER IS IN SWAMPS AND WETLANDS.
NAME CLASS
% OF OUR LIQUID SURFACE
LAKES AND RIVERS HOLD LAKES AND RIVERS HOLD %
% of Earth s Water is fresh water.
%
%
%
%
%
%
%
Surface water is % of Earth s Water. That is 1/3 of %. all THE Lakes, Rivers, and swamps
make that %.
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NAME CLASS
!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""
68% OF EARTH S FRESH WATER IS FROZEN IN GLACIERS AND ICE CAPS.
A little over 30% OF EARTH S FRESH WATER IS GROUNDWATER . about .9% is Other surface water.(not Shown on
the graph).
LAKES AND RIVERS HOLD 89% OF OUR LIQUID SURFACE WATER.
97% OF EARTH S WATER IS SALT WATER IN THE OCEAN.
.001% OF EARTH S WATER IS IN THE ATMOSPHERE.
11% OF OUR LIQUID SURFACE WATER IS IN SWAMPS AND WETLANDS.
NAME CLASS
3% of Earth s Water is fresh water.
Surface water is .3% of Earth s Water. That is 1/3 of 1%. all THE Lakes, Rivers, and swamps combined make that .3%.
97%
3%
68%
30%
.3%
89%
11%
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WATER MOLECULES ARE POLAR. THAT MEANS THEY HAVE POLES LIKE A MAGNET. The oxygen end is slightly negative. The hydrogen end is slightly positive. POLARITY HAS AN EFFECT ON OTHER PROPERTIES OF WATER.
IT TAKES A LOT OF HEAT ENERGY TO RAISE THE TEMPERATURE OF WATER AND WATER HOLDS ONTO HEAT ENERGY BETTER THAN OTHER SUBSTANCES.
EARTH S SEASONS CHANGE GRADUALLY BECAUSE OF the amount of water in the ocean and its influence on temperature.
Water molecules stick to other polar substances like glass. It s why you see a curve at the surface of water when you look at it in a test tube. It s why water sticks to windows.
WATER MOLECULES also STICK TO EACH OTHER. That HELPS WATER Move against gravity up the stems of plants. It also makes them stick close together at the surface of water.
MOST SUBSTANCES SHRINK WHEN COLD. WATER DOES THE OPPOSITE. THIS PROPERTY OF WATER MAKES ICE LESS DENSE THAN LIQUID water. This property is related to polarity of the water molecule.
At low temperatures we get stuck in a rigid formation with space in the middle so ice is less dense than water.
The positive and negative poles of water molecules make it easy for other molecules to dissolve (form new bonds) in water. Here you see an atom of sodium (+) with a positive charge, surrounded by four water molecules.
OH H ;"
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NAME CLASS
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WATER MOLECULES ARE THAT MEANS THEY HAVE POLES LIKE A MAGNET. The end is slightly
. The hydrogen end is slightly ..
HAS AN EFFECT ON OTHER PROPERTIES OF WATER.
IT TAKES A LOT OF ENERGY TO RAISE THE OF WATER AND WATER HOLDS ONTO HEAT ENERGY BETTER THAN OTHER SUBSTANCES.
EARTH S
CHANGE GRADUALLY BECAUSE OF the amount of
in the ocean and its influence on temperature.
Water molecules stick to other substances like glass.
It s why you see a curve at the surface of water when you look at it in a test tube. It s why water sticks to windows.
WATER MOLECULES also STICK TO . That HELPS
WATER MOVE against gravity UP THE STEMS OF PLANTS. It also makes them stick close together at the of water.
MOST SUBSTANCES WHEN COLD. WATER DOES THE OPPOSITE. THIS PROPERTY OF WATER MAKES ICE DENSE THAN LIQUID water. This property is related to polarity of the water molecule.
At temperatures we get stuck in a rigid formation with space in the middle so ice is less than water.
The positive and negative poles of water molecules make it easy for other molecules to (form new bonds) in water. Here you see an atom of (+) with a positive charge, surrounded by four water molecules.
OH H ;"
< <
;"
<" <"
<"<"
;"
;"<"
<"
;"
<" <"
;"<" <"
;"
;"
;"<"
<"
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<"
NAME CLASS
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OH H ;"
< <
;"
<" <"
<"<"
;"
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;"<"
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NAME CLASS
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WATER MOLECULES ARE POLAR. THAT MEANS THEY HAVE POLES LIKE A MAGNET. The oxygen end is slightly negative. The hydrogen end is slightly positive. POLARITY HAS AN EFFECT ON OTHER PROPERTIES OF WATER.
IT TAKES A LOT OF HEAT ENERGY TO RAISE THE TEMPERATURE OF WATER AND WATER HOLDS ONTO HEAT ENERGY BETTER THAN OTHER SUBSTANCES.
EARTH S SEASONS CHANGE GRADUALLY BECAUSE OF the amount of water in the ocean and its influence on temperature.
Water molecules stick to other polar substances like glass. It s why you see a curve at the surface of water when you look at it in a test tube. It s why water sticks to windows.
WATER MOLECULES also STICK TO EACH OTHER. That HELPS WATER MOVE UP THE STEMS OF PLANTS AGAINST GRAVITY. It also makes them stick close together at the surface of water.
MOST SUBSTANCES SHRINK WHEN COLD. WATER DOES THE OPPOSITE. THIS PROPERTY OF WATER MAKES ICE LESS DENSE THAN LIQUID water. This property is related to polarity of the water molecule.
At low temperatures we get stuck in a rigid formation with space in the middle so ice is less dense than water.
The positive and negative poles of water molecules make it easy for other molecules to dissolve (form new bonds) in water. Here you see an atom of sodium (+) with a positive charge, surrounded by four water molecules.
OH H ;"
< <
;"
<" <"
<"<"
;"
;"<"
<"
;"
<" <";"
<" <"
<"
<";"
;"<" <"
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<"<"
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<"
water.
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NAME CLASS
EVAPORATION EVAPORATION
condensation condensation
Precipitation Precipitation
transpiration and respiration and respiration
Infiltration Infiltration
Runoff
water droplets fall as rain, snow, sleet, or hail.
water vapor is
released by plants
and animals by
evaporation .
Water from
precipitation and
melting snow and ice
sinks into the soil and
eventually flows into
rivers, lakes, and
oceans.
Water from melting snow and ice
flows into rivers, and then into
lakes and oceans.
Surface water heated
by the sun becomes
water vapor and rises.
Water vapor rises and
cools forming visible
droplets seen as
clouds.
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NAME CLASS
water droplets fall as ,
, , or .
is
released by plants
and animals by
.
Water from
and
melting snow and ice
sinks into the
and eventually flows
into , ,
and .
Water from melting snow and ice
flows into , and then
into and .
water heated
by the sun becomes
water and
rises.
Water vapor rises and
cools forming
seen as
.
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NAME CLASS
!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""
NAME CLASS
EVAPORATION EVAPORATION
condensation condensation
Precipitation Precipitation
transpiration and respiration and respiration
Infiltration Infiltration
Runoff
water droplets fall as rain, snow, sleet, or hail.
water vapor is
released by plants
and animals by
evaporation .
Water from
precipitation and
melting snow and ice
sinks into the soil and
eventually flows into
rivers, lakes, and
oceans.
Water from melting snow and ice
flows into rivers, and then into
lakes and oceans.
surface water heated
by the sun becomes
water vapor and rises.
Water vapor rises and
cools forming visible
droplets seen as
clouds.
!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""
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Credits Except as noted below, all parts of this resource are the work of the author."=&7">%87"0$-7"?(1$)"%67"$&7"@(6A"(?"B.C,76-D"E7)@7.1"%$"""&F>)GHH@@@2$7%/&76)>%D$7%/&76)2/(CHI$(67HB.C,76-D;E7)@7.1;J(1$)""""=&7"8-(,7".)"$&7"@(6A"(?"*&($(5-.>K"%$G"&F>)GHH@@@2$7%/&76)>%D$7%/&76)2/(CHI$(67H*&($(;5-.>K""=&7"@%$76"/D/-7"7%6$&".--+)$6%0(1".)""$&7"@(6A"(?"I%6%&"*7/(6.1("%$G"&F>)GHH@@@2$7%/&76)>%D$7%/&76)2/(CHI$(67HI%6%&;*7/(6.1(;L--+)$6%0(1""""