Using SST values, how is heat moved from the equatorial region to the north Atlantic Ocean? a.Gulf Stream current b.Equatorial current c.El Nino d.Kuroshio current

Applications and Investigations in Earth Science (9th Edition)
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Using SST values, how is heat moved from the equatorial region to the north Atlantic Ocean?

a.Gulf Stream current
b.Equatorial current
c.El Nino
d.Kuroshio current

Relatively warm tropical ocean water is the source of the latent heat energy that sustains hurricanes and tropical storms. Examine Figures 4B-2 and 4B-3. Which areas are best suited for the storms to form?

a.Equatorial Atlantic Ocean in February.
b.Equatorial Atlantic Ocean in August.
c.North Atlantic Ocean in February.
d.North Atlantic Ocean in August.

68
World Ocean Atlas Climatology
Decadal average: 1955 - 2017
Contour Interval-2
Zoom In
60°E
120°E
180
120'W
60°W
90'N-
-90'N
30
60'N-
60'N
24
30'N-
30'N
18
4.0
12
30°S-
30'S
60'S-
+60'S
60°E
120°E
180
120'W
60 W
Figure 4B-2. February mean sea-surface temperatures in °C. [World Ocean Atlas 2018]
World Ocean Atlas Climatology
Decadal average: 1955 - 2017
Contour Interval-2
60'E
120'E
180
120'W
60 W
90'N-
-90'N
30
60'N-
60'N
24
30°N-
-30'N
18
12
30°S-
30'S
60's
60'S
60'E
120'E
180
120 w
60'w
Transcribed Image Text:68 World Ocean Atlas Climatology Decadal average: 1955 - 2017 Contour Interval-2 Zoom In 60°E 120°E 180 120'W 60°W 90'N- -90'N 30 60'N- 60'N 24 30'N- 30'N 18 4.0 12 30°S- 30'S 60'S- +60'S 60°E 120°E 180 120'W 60 W Figure 4B-2. February mean sea-surface temperatures in °C. [World Ocean Atlas 2018] World Ocean Atlas Climatology Decadal average: 1955 - 2017 Contour Interval-2 60'E 120'E 180 120'W 60 W 90'N- -90'N 30 60'N- 60'N 24 30°N- -30'N 18 12 30°S- 30'S 60's 60'S 60'E 120'E 180 120 w 60'w
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