Wikipedia

Walker circulation

The Walker circulation, also known as the Walker cell, is a conceptual model of the air flow in the tropics in the lower atmosphere (troposphere). According to this model, parcels of air follow a closed circulation in the zonal and vertical directions. This circulation, which is roughly consistent with observations, is caused by differences in heat distribution between ocean and land. In addition to motions in the zonal and vertical direction the tropical atmosphere also has considerable motion in the meridional direction as part of, for example, the Hadley Circulation.

A schematic diagram of the quasi-equilibrium and La Niña phase of the southern oscillation. The Walker circulation is seen at the surface as easterly trade winds which move water and air warmed by the sun towards the west. The western side of the equatorial Pacific is characterized by warm, wet low pressure weather as the collected moisture is dumped in the form of typhoons and thunderstorms. The ocean is some 60 cm higher in the western Pacific as the result of this motion. The water and air are returned to the east. Both are now much cooler, and the air is much drier. An El Niño episode is characterised by a breakdown of this water and air cycle, resulting in relatively warm water and moist air in the eastern Pacific.

The Walker circulation is associated with the pressure gradient force that results from a high pressure system over the eastern Pacific Ocean, and a low pressure system over Indonesia. The Walker circulations of the tropical Indian, Pacific, and Atlantic basins result in westerly surface winds in northern summer in the first basin and easterly winds in the second and third basins. As a result, the temperature structure of the three oceans display dramatic asymmetries. The equatorial Pacific and Atlantic both have cool surface temperatures in northern summer in the east, while cooler surface temperatures prevail only in the western Indian Ocean.[1] These changes in surface temperature reflect changes in the depth of the thermocline.[2]

Changes in the Walker circulation with time occur in conjunction with changes in surface temperature. Some of these changes are forced externally, such as the seasonal shift of the sun into the Northern Hemisphere in summer. Other changes appear to be the result of coupled ocean-atmosphere feedback in which, for example, easterly winds cause the sea surface temperature to fall in the east, enhancing the zonal heat contrast and hence intensifying easterly winds across the basin. These anomalous easterlies induce more equatorial upwelling and raise the thermocline in the east, amplifying the initial cooling by the southerlies. From an oceanographic point of view, the equatorial cold tongue is caused by easterly winds. Were the Earth climate symmetric about the equator, cross-equatorial wind would vanish, and the cold tongue would be much weaker and have a very different zonal structure than is observed today.[3]

The Walker circulation was discovered by Gilbert Walker. The term "Walker circulation" was coined in 1969 by the Norwegian-American meteorologist Jacob Bjerknes.[4]

Walker's methodology

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Gilbert Walker was an established applied mathematician at the University of Cambridge when he became director-general of observatories in India in 1904.[5] While there, he studied the characteristics of the Indian Ocean monsoon, the failure of whose rains had brought severe famine to the country in 1899. Analyzing vast amounts of weather data from India and the rest of the world, over the next fifteen years he published the first descriptions of the great seesaw oscillation of atmospheric pressure between the Indian and Pacific Ocean, and its correlation to temperature and rainfall patterns across much of the Earth's tropical regions, including India. He also worked with the Indian Meteorological Department especially in linking the monsoon with Southern Oscillation phenomenon. He was made a Companion of the Order of the Star of India in 1911.[5]

Walker determined that the time scale of a year (used by many studying the atmosphere) was unsuitable because geospatial relationships could be entirely different depending on the season. Thus, Walker broke his temporal analysis into December–February, March–May, June–August, and September–November.

Walker then selected a number of "centers of action", which included areas such as the Indian Peninsula. The centers were in the hearts of regions with either permanent or seasonal high and low pressures. He also added points for regions where rainfall, wind or temperature was an important control.

He examined the relationships of the summer and winter values of pressure and rainfall, first focusing on summer and winter values, and later extending his work to the spring and autumn.

He concludes that variations in temperature are generally governed by variations in pressure and rainfall. It had previously been suggested that sunspots could be the cause of the temperature variations, but Walker argued against this conclusion by showing monthly correlations of sunspots with temperature, winds, cloud cover, and rain that were inconsistent.

Walker made it a point to publish all of his correlation findings, both of relationships found to be important as well as relationships that were found to be unimportant. He did this for the purpose of dissuading researchers from focusing on correlations that did not exist.

Oceanic effects

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Average equatorial Pacific temperatures
 
Graph showing a tropical ocean thermocline (depth vs. temperature). Note the rapid change between 100 and 1000 meters. The temperature is nearly constant after 1500 meters depth.

The Walker Circulations of the tropical Indian, Pacific, and Atlantic basins result in westerly surface winds in Northern Summer in the first basin and easterly winds in the second and third basins. As a result, the temperature structure of the three oceans display dramatic asymmetries. The equatorial Pacific and Atlantic both have cool surface temperatures in Northern Summer in the east, while cooler surface temperatures prevail only in the western Indian Ocean.[6] These changes in surface temperature reflect changes in the depth of the thermocline.[7]

Changes in the Walker Circulation with time occur in conjunction with changes in surface temperature. Some of these changes are forced externally, such as the seasonal shift of the Sun into the Northern Hemisphere in summer. Other changes appear to be the result of coupled ocean-atmosphere feedback in which, for example, easterly winds cause the sea surface temperature to fall in the east, enhancing the zonal heat contrast and hence intensifying easterly winds across the basin. These enhanced easterlies induce more equatorial upwelling and raise the thermocline in the east, amplifying the initial cooling by the southerlies. This coupled ocean-atmosphere feedback was originally proposed by Bjerknes. From an oceanographic point of view, the equatorial cold tongue is caused by easterly winds. Were the earth climate symmetric about the equator, cross-equatorial wind would vanish, and the cold tongue would be much weaker and have a very different zonal structure than is observed today.[8] The Walker cell is indirectly related to upwelling off the coasts of Peru and Ecuador. This brings nutrient-rich cold water to the surface, increasing fishing stocks.[9]

El Niño–Southern Oscillation

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Main article: El Niño–Southern Oscillation

The Walker circulation is caused by the pressure gradient force that results from a high pressure system over the eastern Pacific Ocean and a low pressure system over Indonesia. The Walker circulation causes an upwelling of cold deep sea water, thus cooling the sea surface. El Niño results when this circulation decreases or stops, as the impaired or inhibited circulation causes the ocean surface to warm to above average temperatures. A markedly increased Walker circulation causes a La Niña by intensifying the upwelling of cold deep sea water; which cools the sea surface to below average temperatures.

During non-El Niño conditions, the Walker circulation is seen at the surface as easterly trade winds that move water and air warmed by the sun toward the west. This also creates ocean upwelling off the coasts of Peru and Ecuador and brings nutrient-rich cold water to the surface, increasing fishing stocks.[10] The western side of the equatorial Pacific is characterized by warm, wet, low-pressure weather as the collected moisture is dumped in the form of typhoons and thunderstorms. The ocean is some 60 cm (24 in) higher in the western Pacific as the result of this motion.[11][12][13][14]

A scientific study published in May 2006 in the journal Nature indicates that the Walker circulation has been slowing since the mid-19th century. The authors argue that global warming is a likely causative factor in the weakening of the wind pattern.[15] However, a 2011 study from The Twentieth Century Reanalysis Project shows that, aside from El Niño–Southern Oscillation cycles, the overall speed and direction of the Walker circulation remained steady between 1871 and 2008.[16]

See also

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References

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  1. ^ Bureau of Meteorology. "The Walker Circulation". Commonwealth of Australia. Retrieved 1 July 2014.
  2. ^ Zelle, Hein; Gerrian Appledoorn; Gerritt Burgers; Geert Jan Van Oldenborgh (2004). "Relationship Between Sea Surface Temperature and Thermocline Depth in the Eastern Equatorial Pacific". Journal of Physical Oceanography. 34 (3): 643–655. Bibcode:2004JPO....34..643Z. CiteSeerX 10.1.1.12.3536. doi:10.1175/2523.1. S2CID 16785385.
  3. ^ Xie, Shang-Ping (1 February 1998). "Ocean-Atmosphere Interaction in the Making of the Walker Circulation and Equatorial Cold Tongue". Journal of Climate. 11 (2): 189–201. Bibcode:1998JCli...11..189X. doi:10.1175/1520-0442(1998)011<0189:OAIITM>2.0.CO;2. JSTOR 26242917. INIST 2154325.
  4. ^ Bjerknes, J. (March 1969) "Atmospheric teleconnections from the equatorial Pacific," Monthly Weather Review, 97 (3) : 163–172. From pp. 167–168: "It seems reasonalble to assume that it is the gradient of sea temperature along the Equator which is the cause of the thermal circulation entered in figure 8. Hereafter, in the present article that circulation will be referred to as the "Walker Circulation" since it can be shown to be an important part of the mechanism of Walker's "Southern Oscillation." " Available at: N.O.A.A.
  5. ^ a b Rao, C. Hayavadana, ed. (1915). "Walker, Gilbert Thomas" . The Indian Biographical Dictionary . Vol. 24.1. Madras: Pillar & Co. p. 456.
  6. ^ Bureau of Meteorology. "The Walker Circulation". Commonwealth of Australia. Retrieved 1 July 2014.
  7. ^ Zelle, Hein, Gerrian Appledoorn, Gerritt Burgers, and Gert Jan Van Oldenborgh (March 2004). "Relationship Between Sea Surface Temperature and Thermocline Depth in the Eastern Equatorial Pacific". Journal of Physical Oceanography. 34 (3): 643. Bibcode:2004JPO....34..643Z. CiteSeerX 10.1.1.12.3536. doi:10.1175/2523.1. S2CID 16785385.{{cite journal}}: CS1 maint: multiple names: authors list (link)
  8. ^ Ocean-atmosphere interaction in the making of the Walker circulation and equatorial cold tongue
  9. ^ Jennings, S., Kaiser, M.J., Reynolds, J.D. (2001) "Marine Fisheries Ecology." Oxford: Blackwell Science Ltd. ISBN 0-632-05098-5
  10. ^ Jennings, S., Kaiser, M.J., Reynolds, J.D. (2001) "Marine Fisheries Ecology." Oxford: Blackwell Science Ltd. ISBN 0-632-05098-5[page needed]
  11. ^ Pidwirny, Michael (2 February 2006). "Chapter 7: Introduction to the Atmosphere". Fundamentals of Physical Geography. physicalgeography.net. Retrieved 30 December 2006.
  12. ^ "Envisat watches for La Niña". BNSC via the Internet Wayback Machine. 9 January 2011. Archived from the original on 24 April 2008. Retrieved 26 July 2007.
  13. ^ "The Tropical Atmosphere Ocean Array: Gathering Data to Predict El Niño". Celebrating 200 Years. NOAA. 8 January 2007. Retrieved 26 July 2007.
  14. ^ "Ocean Surface Topography". Oceanography 101. JPL. 5 July 2006. Archived from the original on 14 April 2009. Retrieved 26 July 2007."Annual Sea Level Data Summary Report July 2005 – June 2006" (PDF). The Australian Baseline Sea Level Monitoring Project. Bureau of Meteorology. Archived from the original (PDF) on 7 August 2007. Retrieved 26 July 2007.
  15. ^ Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing
  16. ^ The Twentieth Century Reanalysis Project. Quarterly Journal of the Royal Meteorological Society, 137: 1–28. doi:10.1002/qj.776, http://onlinelibrary.wiley.com/doi/10.1002/qj.776/abstract

General references

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