Ocean
Temperature
Warmer
oceans put coastal communities at risk, increase infrastructure costs, endanger
polar creatures and threaten coral reefs and fisheries. Perhaps most alarmingly,
rising ocean temperatures accelerate the overall warming trend.
Not only are ocean surface waters getting warmer, but so is
water 1,500 feet below the surface. These increases in temperature lie well
outside the bounds of natural variation.
In fact, the ocean has absorbed so much heat—about 20 times as
much as the atmosphere over the past half-century—that some models suggest that
it is likely to warm the air another degree Fahrenheit (0.55° Celsius)
worldwide over the coming decades.
Although ocean temperatures are more difficult to measure than
land temperatures, scientists can use several methods to create an extensive
ocean record.
- Dropped
from ships or airplanes, probes gauging the ocean's conductivity,
temperature, and density provide nearly continuous surface-to-bottom
measurements at specific times. However, these probes rarely reoccupy an
exact location.
- Remote
vehicles can measure the temperature of deep ocean waters, and
periodically surface to transfer the information to satellites.
- Moorings
on the ocean bottom can measure temperatures at fixed distances above the
bottom, until a ship retrieves the instruments—typically after a few
months or years.
- The
most common measurements, however, are taken at the sea surface.
Scientists combine these measurements with land surface measurements to
calculate the global average temperature.
- Scientists
also know that ocean temperatures are rising because warm-water species
are moving into areas that were formerly too cold, while cool-water and
cold-water species are likewise on the move.
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