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Why Atmospheric Pressure Peaks At 10am And 10pm In The Tropics

Date:
December 14, 2008
Source:
University of Hawaii at Manoa
Summary:
For over two centuries, meteorologists were puzzled by the observation that atmospheric pressure in the tropics peaks at 10 a.m. and 10 p.m. nearly every day.
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FULL STORY

Steve Ryan and Kevin Hamilton inspect one of the atmospheric pressure sensors at the Mauna Loa Observatory.
Credit: The International Pacific Research Center, UH Manoa

For over two centuries, meteorologists were puzzled by the observation that atmospheric pressure in the tropics peaks at 10 a.m. and 10 p.m. nearly every day. In the late 1960s, a theory was proposed that these surface pressure variations result from waves that are generated by the sun's heating of the upper atmosphere.

The waves, called solar tides, propagate to the ground as they travel around the globe. Strong support for this theory has now been presented in a study by a US-Japan team of scientists spearheaded by University of Hawai'i (UH) Professor Kevin Hamilton, Interim Director of the UH climate research center, the International Pacific Research Center.

Hamilton reasoned that if the proposed explanation was correct, then the pressure variations should be affected systematically by topography. Since mountains cast a kind of shadow for the atmospheric wave as it propagates westward (following the sun) and downward, he predicted that the pressure variations should be weaker on the west than the east side of steep mountains.

Working with Wataru Ohfuchi of the Japanese Earth Simulator Center in Yokohama, Hamilton was able to show that this topographic effect is seen in very sophisticated computer model simulations of the global atmosphere.

One of the most dramatic examples of the shadow effect in the computer model results occurs with the tall mountains of the Big Island of Hawaii. Fortunately, the Mauna Loa Observatory (MLO) had deployed a network of pressure sensors on the Big Island in 2004. Together with MLO scientist Steve Ryan, Hamilton was able to show that the shadow effect is seen in these real pressure observations as well [photo: Ryan and Hamilton (right)].

The Hawaii results thus shed light on an important feature of the global atmosphere.

The International Pacific Research Center (IPRC) of the School of Ocean and Earth Science at UH Manoa conducts research to gain greater understanding of the climate system, the nature and causes of climate variations in the Asia-Pacific region, and how global climate changes may affect the region. Established under the "U.S.-Japan Common Agenda for Cooperation in Global Perspective" in October 1997, the IPRC is a collaborative effort between the UH and agencies in Japan and the United States.


Story Source:

The above story is based on materials provided by University of Hawaii at Manoa. Note: Materials may be edited for content and length.


Journal Reference:

  1. Hamilton, K., S. C. Ryan, and W. Ohfuchi. Topographic effects on the solar semidiurnal surface tide simulated in a very fine resolution general circulation model. Journal of Geophysical Research - Atmospheres, 113, D17114 DOI: 10.1029/2008JD010115

Cite This Page:

University of Hawaii at Manoa. "Why Atmospheric Pressure Peaks At 10am And 10pm In The Tropics." ScienceDaily. ScienceDaily, 14 December 2008. <www.sciencedaily.com/releases/2008/12/081203092437.htm>.
University of Hawaii at Manoa. (2008, December 14). Why Atmospheric Pressure Peaks At 10am And 10pm In The Tropics. ScienceDaily. Retrieved May 22, 2015 from www.sciencedaily.com/releases/2008/12/081203092437.htm
University of Hawaii at Manoa. "Why Atmospheric Pressure Peaks At 10am And 10pm In The Tropics." ScienceDaily. www.sciencedaily.com/releases/2008/12/081203092437.htm (accessed May 22, 2015).

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