Sudden stratospheric warming

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A sudden stratospheric warming (SSW) is an event where the polar vortex of westerly winds in the winter hemisphere slows down or even reverses direction over the course of a few days. The change is accompanied by a rise of stratospheric temperature by several tens of kelvins.


The first continuous measurements of the stratosphere were taken by Richard Scherhag in 1951. He used radiosondes to take reliable temperature readings in the upper stratosphere (~40 km). It was his persistence which led him to witness the first ever observed stratospheric warming on 27 January 1952. After his discovery, Scherhag assembled a team of meteorologists specifically to study the stratosphere at the Free University of Berlin. This group continued to map the northern-hemisphere stratospheric temperature and geopotential height for many years using radiosondes and rocketsondes. In 1979 when the satellite era began, meteorological measurements became far more frequent. Although satellites were primarily used for the troposphere they also recorded data for the stratosphere. Today both satellites and stratospheric radiosondes are used to take measurements of the stratosphere.

Classification and description[edit]

Typically stratospheric meteorologists classify the vortex breakdown into three categories: major, minor, and final.

Sometimes a fourth category, the Canadian warming, is included because of its unique and distinguishing structure and evolution.


These occur when the westerly winds at 60N and 10hPa (geopotential height) reverse, i.e. become easterly. A complete disruption of the polar vortex is observed and the vortex will either be split into daughter vortices, or displaced from its normal location over the pole.

According to the World Meteorological Organization's Commission for Atmospheric Sciences (Mclnturff, 1978): a stratospheric warming can be said to be major if 10 mb or below the latitudinal mean temperature increases poleward from 60 degree latitude and an associated circulation reversal is observed (that is, the prevailing mean westerly winds poleward of 60 latitude are succeeded by mean easterlies in the same area).


Minor warmings are similar to major warmings however they are less dramatic, the westerly winds are slowed, however do not reverse. Therefore a breakdown of the vortex is never observed.

Mclnturff states: a stratospheric warming is called minor if a significant temperature increase is observed (that is, at least 25 degrees in a period of week or less) at any stratospheric level in any area of winter time hemisphere. The polar vortex is not broken down and the wind reversal from westerly to easterly is less extensive.


The radiative cycle in the stratosphere means that during winter the mean flow is westerly and during summer it is easterly (westward). A final warming occurs on this transition, so that the polar vortex winds change direction for the warming, however do not change back until the following winter. This is because the stratosphere has entered the summer easterly phase. It is final because another warming cannot occur over the summer, so it is the final warming of the current winter.


Canadian warmings occur in early winter in the stratosphere of the Northern Hemisphere, typically from mid November to early December. They have no counterpart in the southern hemisphere.


In a usual northern-hemisphere winter, several minor warming events occur, with a major event occurring roughly every two years. One reason for major stratospheric warmings to occur in the Northern hemisphere is because orography and land-sea temperature contrasts are responsible for the generation of long (wavenumber 1 or 2) Rossby waves in the troposphere. These waves travel upward to the stratosphere and are dissipated there, decelerating the winds and warming the Arctic. This is the reason that major warmings are only observed in the northern-hemisphere, with one exception. In 2002 a southern-hemisphere major warming was observed.[1] This event to date is not fully understood.

At an initial time a blocking-type circulation pattern establishes in the troposphere. This blocking pattern causes[clarification needed] Rossby waves with zonal wavenumber 1 and/or 2[clarification needed] to grow to unusually large amplitudes. The growing wave propagates into the stratosphere and decelerates the mean zonal winds.[clarification needed] Thus the polar night jet weakens and simultaneously becomes distorted by the growing planetary waves. Because the wave amplitude increases with decreasing density this easterly acceleration process is not effective at fairly high levels.[why?] If the waves are sufficiently strong the mean zonal flow may decelerate sufficiently so that the winter westerlies turn easterly. At this point planetary waves may no longer penetrate into the stratosphere [2][clarification needed]). Hence further upward transfer of energy is completely blocked and a very rapid easterly deceleration and the polar warming occur at this critical level, which must then move downward until eventually the warming and zonal wind reversal affect the entire polar stratosphere.

There exists a link between sudden stratospheric warmings and the quasi-biennial oscillation: If the QBO is in its easterly (westward) phase, the atmospheric waveguide is modified in such a way that upward-propagating Rossby waves are focused on the polar vortex, intensifying their interaction with the mean flow. Thus, there exists a statistically significant imbalance between the frequency of sudden stratospheric warmings if these events are grouped according to the QBO phase (easterly or westerly).

Weather effects[edit]

Although sudden stratospheric warmings are mainly forced by planetary scale waves which propagate up from the lower atmosphere, there is also a subsequent return effect of sudden stratospheric warmings on surface weather. Following a sudden stratospheric warming, the high altitude winds reverse to flow eastward instead of their usual westward. The eastward winds progress down through the atmosphere and weaken the jet stream, often giving westward winds near the surface and resulting in dramatic reductions in temperature in the Eastern U.S. and Europe.

See also[edit]


  1. ^ Manney, Gloria L.; Sabutis, Joseph L.; Allen, Douglas R.; Lahoz, William A.; Scaife, Adam A.; Randall, Cora E.; Pawson, Steven; Naujokat, Barbara; Swinbank, Richard (2005). "Simulations of Dynamics and Transport during the September 2002 Antarctic Major Warming". Journal of the Atmospheric Sciences 62 (3): 690. doi:10.1175/JAS-3313.1. 
  2. ^ Charney, J. G.; Drazin, P. G. (1961). "Propagation of planetary-scale disturbances from the lower into the upper atmosphere". Journal of Geophysical Research 66: 83. doi:10.1029/JZ066i001p00083. 

Further reading[edit]

  • Dowdy, Andrew et al. (2004). "The large-scale dynamics of the mesosphere-lower thermosphere during the Southern Hemisphere stratospheric warming of 2002". Geophys. Res. Lett 31: L14102. doi:10.1029/2004GL020282. 
  • Dowdy, Andrew et al. (2007). "Polar mesosphere and lower thermosphere dynamics:2. Response to sudden stratospheric warmings". J. Geophys. Res 112: D17105. doi:10.1029/2006JD008127. 
  • Matsuno, Taroh (1971). "A Dynamical Model of the Stratospheric Sudden Warming". Journal of the Atmospheric Sciences 28 (8): 1479–94. Bibcode:1971JAtS...28.1479M. doi:10.1175/1520-0469(1971)028<1479:ADMOTS>2.0.CO;2. 
  • McGuirk, James P.; Douglas, Donald A. (1988). "Sudden Stratospheric Warming and Anomalous U.S. Weather". Monthly Weather Review 116: 162. Bibcode:1988MWRv..116..162M. doi:10.1175/1520-0493(1988)116<0162:SSWAAU>2.0.CO;2. 
  • Liu, H.-L.; Roble, R. G. (2002). "A study of a self-generated stratospheric sudden warming and its mesospheric–lower thermospheric impacts using the coupled TIME-GCM/CCM3". Journal of Geophysical Research 107: 4695. Bibcode:2002JGRD..107.4695L. doi:10.1029/2001JD001533. 
  • Limpasuvan, Varavut; Thompson, David W. J.; Hartmann, Dennis L. (2004). "The Life Cycle of the Northern Hemisphere Sudden Stratospheric Warmings". Journal of Climate 17 (13): 2584–96. doi:10.1175/1520-0442(2004)017<2584:TLCOTN>2.0.CO;2. 
  • Manney, Gloria L.; Krüger, Kirstin; Sabutis, Joseph L.; Sena, Sara Amina; Pawson, Steven (2005). "The remarkable 2003–2004 winter and other recent warm winters in the Arctic stratosphere since the late 1990s". Journal of Geophysical Research 110: 4107. Bibcode:2005JGRD..110.4107M. doi:10.1029/2004JD005367. 
  • Nakagawa, Ken I.; Yamazaki, Koji (2006). "What kind of stratospheric sudden warming propagates to the troposphere?". Geophysical Research Letters 33 (4): 4801. Bibcode:2006GeoRL..33.4801N. doi:10.1029/2005GL024784. 
  • Taguchi, Masakazu; Hartmann, Dennis L. (2006). "Increased Occurrence of Stratospheric Sudden Warmings during El Niño as Simulated by WACCM". Journal of Climate 19 (3): 324. Bibcode:2006JCli...19..324T. doi:10.1175/JCLI3655.1. 
  • Charlton, Andrew J.; Polvani, Lorenzo M. (2007). "A New Look at Stratospheric Sudden Warmings. Part I: Climatology and Modeling Benchmarks". Journal of Climate 20 (3): 449. Bibcode:2007JCli...20..449C. doi:10.1175/JCLI3996.1. 
  • Charlton, Andrew J.; Polvani, Lorenzo M.; Perlwitz, Judith; Sassi, Fabrizio; Manzini, Elisa; Shibata, Kiyotaka; Pawson, Steven; Nielsen, J. Eric; Rind, David (2007). "A New Look at Stratospheric Sudden Warmings. Part II: Evaluation of Numerical Model Simulations". Journal of Climate 20 (3): 470. Bibcode:2007JCli...20..470C. doi:10.1175/JCLI3994.1. 
  • Peters, Dieter; Vargin, Pawel; Körnich, Heiner (2007). "A Study of the zonally asymmetric tropospheric forcing of the austral vortex splitting during September 2002". Tellus A 59 (3): 384–94. Bibcode:2007TellA..59..384P. doi:10.1111/j.1600-0870.2007.00228.x. 
  • Stan, Cristiana; Straus, David M. (2009). "Stratospheric predictability and sudden stratospheric warming events". Journal of Geophysical Research 114: 12103. Bibcode:2009JGRD..11412103S. doi:10.1029/2008JD011277. 
  • Matthewman, N. J.; Esler, J. G.; Charlton-Perez, A. J.; Polvani, L. M. (2009). "A New Look at Stratospheric Sudden Warmings. Part III: Polar Vortex Evolution and Vertical Structure". Journal of Climate 22 (6): 1566. Bibcode:2009JCli...22.1566M. doi:10.1175/2008JCLI2365.1. 
  • Evers, L. G.; Siegmund, P. (2009). "Infrasonic signature of the 2009 major sudden stratospheric warming". Geophysical Research Letters 36 (23): 23808. Bibcode:2009GeoRL..3623808E. doi:10.1029/2009GL041323. 
  • Martineau, Patrick; Son, Seok-Woo (2010). "Quality of reanalysis data during stratospheric vortex weakening and intensification events". Geophysical Research Letters 37 (22): n/a. Bibcode:2010GeoRL..3722801M. doi:10.1029/2010GL045237. 
  • Peters, D. H. W.; Vargin, P.; Gabriel, A.; Tsvetkova, N.; Yushkov, V. (2010). "Tropospheric forcing of the boreal polar vortex splitting in January 2003". Annales Geophysicae 28 (11): 2133. Bibcode:2010AnGeo..28.2133P. doi:10.5194/angeo-28-2133-2010. 
  • Fuller-Rowell, Tim; Akmaev, Rashid; Wu, Fei; Fedrizzi, Mariangel; Viereck, Rodney A.; Wang, Houjun (2011). "Did the January 2009 sudden stratospheric warming cool or warm the thermosphere?". Geophysical Research Letters 38 (18): n/a. Bibcode:2011GeoRL..3818104F. doi:10.1029/2011GL048985. 
  • Ayarzagüena, Blanca; Langematz, Ulrike; Serrano, Encarna (2011). "Tropospheric forcing of the stratosphere: A comparative study of the two different major stratospheric warmings in 2009 and 2010". Journal of Geophysical Research 116: 18114. Bibcode:2011JGRD..11618114A. doi:10.1029/2010JD015023. 
  • Liu, Huixin; Doornbos, Eelco; Yamamoto, Mamoru; Tulasi Ram, S. (2011). "Strong thermospheric cooling during the 2009 major stratosphere warming". Geophysical Research Letters 38 (12): n/a. Bibcode:2011GeoRL..3812102L. doi:10.1029/2011GL047898. 
  • Sun, Lantao; Robinson, Walter A.; Chen, Gang (2012). "The Predictability of Stratospheric Warming Events: More from the Troposphere or the Stratosphere?". Journal of the Atmospheric Sciences 69 (2): 768–83. Bibcode:2012JAtS...69..768S. doi:10.1175/JAS-D-11-0144.1. 
  • Gómez-Escolar, M.; Fueglistaler, S.; Calvo, N.; Barriopedro, D. (2012). "Changes in polar stratospheric temperature climatology in relation to stratospheric sudden warming occurrence". Geophysical Research Letters 39 (22): n/a. Bibcode:2012GeoRL..3922802G. doi:10.1029/2012GL053632. 
  • Ripesi, P.; Ciciulla, F.; Maimone, F.; Pelino, V. (2012). "The February 2010 Artcic Oscillation Index and its stratospheric connection.". Quarterly Journal of the Royal Meteorological Society 138 (669): 1961. doi:10.1002/qj.1935. 

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