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%

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

% 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 %.

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

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%

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

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 ;"

< <

;"

<" <"

<"<"

;"

;"<"

<"

;"

<" <"

;"<" <"

;"

;"

;"<"

<"

;"

<"

NAME CLASS

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

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 ;"

< <

;"

<" <"

<"<"

;"

;"<"

<"

;"

<" <"

;"<" <"

;"

;"

;"<"

<"

;"

<"

NAME CLASS

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

OH H ;"

< <

;"

<" <"

<"<"

;"

;"<"

<"

;"

<" <"

;"<" <"

;"

;"

;"<"

<"

;"

<"

NAME CLASS

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

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 ;"

< <

;"

<" <"

<"<"

;"

;"<"

<"

;"

<" <";"

<" <"

<"

<";"

;"<" <"

;"

<"<"

<"<" ;"

<"

water.

!"#$%&'(($)"*+,-./%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""

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

.

!"#$%&'(($)"*+,-./%0(12"3"42"5&6.)$71)712""!--"'.8&$)"'7)7697:2""

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""

Copyright © Jill Christensen 2018. All rights reserved. Do not provide copies of this digital file to others. Do not upload any part of this digital file to the internet, even to classroom or district websites. Do not upload this file or any part of this file to a server or website where teaching resources are shared without receiving prior permission. Such actions are violations of the Digital Millennium Copyright Act.

The unauthorized reproduction or distribution of a copyrighted work is illegal. Criminal copyright infringement, including infringement without monetary gain, is investigated by the FBI and is punishable by fines and federal imprisonment. La reproducción o distribución no autorizada de una obra protegida por derechos de autor es ilegal. La infracción criminal de los derechos de autor, incluyendo la infracción sin lucro monetario, es investigada por el FBI y es castigable con multas y encarcelamiento federal.

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""""