Weekly Ocean News

26 February-2 March 2018


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Ocean in the News


Concept of the Week: The Ocean and the Global Radiation Budget

The ocean is an important player in the radiational heating and cooling of Planet Earth. For one, covering about 71% of Earth's surface, the ocean is a primary control of how much solar radiation is absorbed (converted to heat) at the Earth's surface. Also, the ocean is the main source of the most important greenhouse gas (water vapor) and is a major regulator of the concentration of atmospheric carbon dioxide (CO2), another greenhouse gas.

On an annual average, the ocean absorbs about 92% of the solar radiation striking its surface; the balance is reflected to space. Most of this absorption takes place within about 200 m (650 ft) of the surface with the depth of penetration of sunlight limited by the amount of suspended particles and discoloration caused by dissolved substances. On the other hand, at high latitudes multi-year pack ice greatly reduces the amount of solar radiation absorbed by the ocean. The snow-covered surface of sea ice absorbs only about 15% of incident solar radiation and reflects away the rest. At present, multi-year pack ice covers about 7% of the ocean surface with greater coverage in the Arctic Ocean than the Southern Ocean (mostly in Antarctica's Weddell Sea).

The atmosphere is nearly transparent to incoming solar radiation but much less transparent to outgoing infrared (heat) radiation. This differential transparency with wavelength is the basis of the greenhouse effect. Certain trace gases in the atmosphere absorb outgoing infrared and radiate some of this energy to Earth's surface, thereby significantly elevating the planet's surface temperature. Most water vapor, the principal greenhouse gas, enters the atmosphere via evaporation of seawater. Carbon dioxide, a lesser greenhouse gas, cycles into and out of the ocean depending on the sea surface temperature and photosynthesis/respiration by marine organisms in surface waters. Cold water can dissolve more carbon dioxide than warm water so that carbon dioxide is absorbed from the atmosphere where surface waters are chilled (at high latitudes and upwelling zones) and released to the atmosphere where surface waters are heated (at low latitudes). Photosynthetic organisms take up carbon dioxide and all organisms release carbon dioxide via cellular respiration.


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Prepared by DS Ocean Central Staff and Edward J. Hopkins, Ph.D.,
email
hopkins@aos.wisc.edu
© Copyright, 2018, The American Meteorological Society.