Earth Science and Society Water Thesis

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The water acquisition in these areas depends specifically on the amount of rain fall. Its climate is affected by the North Pacific High, an oceanic high pressure cell that regulates the moderate temperature ranges. The city lies on the west side of the mountains, so the area receives much more precipitation (University of Illinois 2010). Most Mediterranean climates occur on the Western end of continents. Berkeley, and the entire Californian coast receives most of its rainfall during the winter months, therefore the precipitation rates will be the highest in the winter months than the rest of the year. Moreover, the Ocean regulates temperature in this area, which is completely absent in the case of Terre Haute Indiana. Rather, Berkeley is surrounded by the ocean and mountains, which are the factors that have a primary affect on the differences between the two areas' water budgets.

WATER BUDGET for TERRE HAUTE, INDIANA (Figure 2)

J

F

M

A

M

J

J

A

S

O

N

D

P

7.4

6.8

9.6

9.4

10.1

10.2

8.1

8.2

8.7

6.9

8.4

7.5

PE

0.0

0.0

1.8

4.9

10.2

13.4

15.8

13.8

9.9

5.2

1.7

0.1

P-PE

7.4

6.8

7.8

4.5

0.1

-3.2

-7.7

-5.6

-1.2

1.7

6.7

7.4

Change in ST

0

0

0

0

0

-3.2

-4.5

0

0

1.7

6.7 2.6

ST

10.0

10.
0

10.0

10.0

10.0

6.8

2.3

0

0

1.7

8.4

10

AE

7.4

6.8

9.6

4.5

0.1

-3.2

-7.7

8.2

8.7

6.9

6.7

7.4

D

0

0

0

0

0

0

0

5.6

1.2

0

0

0

S

0

0

0

4.9

10.1

0

0

0

0

0

0

0.1

Terre Haute, Indiana presents much different conditions than Berkeley, California. These differences in conditions are what affect each individual water budget. Terre Haute is a mid-latitude continental climate and sits at 39°28'00.13" N, 87°24'50.07" W. it's elevation is much higher than that of Berkeley's, being about 491 ft above sea level. This altitude change then affects the amount of precipitation the area gets. Terre Haute is far from major mountain ranges, so there is less water transport through run off and snow melt. However, the mountain ranges to the west and south block cold air from leaving the region. According to research, "Moist ocean air masses are blocked by mountain ranges to the west and south. These mountain ranges also trap polar air in winter, making winters very cold," (Schaffner & Robinson 2010). These cold winters are much different than the mild, wet one seen in Berkeley. Since it snows heavily in the winter months, precipitation includes not only rain, but also snow and sleet.

"The agricultural.....

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