Abstract
Fluctuations in the frequency of cyclones in various regions of the Northern Hemisphere (NH) temperate latitudes on time scales of the order of decades are analyzed in connection with changes in the indices of the leading modes of atmospheric circulation and changes in the zonal transport intensity in individual latitudinal zones. The possible manifestation in cyclone statistics of the well-known thesis about the displacement of storm tracks during warming in the direction of high latitudes is discussed. It is shown that, in general, for the NH temperate latitudes in winter, long-period changes in the frequency of cyclones are irregular fluctuations with scales of several decades, without a visible trend. In summer, the interdecade changes are weakly expressed, but there is a noticeable trend that is significant at the 5% level. In the northern and southern parts of the North Atlantic (NA) in winter, changes in frequency contain significant antiphase components with a period of about 10 years, which correlate well with changes in the North Atlantic Oscillation (NAO) index (the correlation is positive in the northern half; the coefficients are significant at the 0.1% level). Long-period changes in the frequency of cyclones in the North Pacific are generally similar to (but in the opposite phase of) changes in the North Pacific Index by Trenberth and Hurrell. Based on the analysis of a linear regression model, it was found that a significant contribution to changes in the frequency of cyclones in the regions of northern Europe–Western Siberia and the north of ER (ER) in the winter season was made by the circulation modes of the Atlantic–European sector: SCAND, NAO, East Atlantic mode EAM, EAWR (but the EAWR mode contribution is insignificant for the north of Europe–Western Siberia). In summer, for the north of ER and Western Siberia, a significant contribution was made by the SCAND and EAWR circulation modes. An analysis of concomitant changes in zonal wind speed at 700 hPa in the area of the main storm tracks in winter revealed that, for the hemisphere as a whole (0°–360°) in the latitude zone 45°–55° N, as well as in the zone 55°–65° N, changes in zonal wind are determined mainly by changes in the frequency of cyclones in the northern part of the NA and closely follow changes in the NAO. However, in more southern latitudes (35°–45° N), changes in the hemispheric zonal wind are observed, similar to long-period changes in the North Pacific Index in antiphase, the nature of which is unclear (since they do not appear in the Pacific sector itself). The shift of storm tracks to higher latitudes, expected with warming, is observed only for the northern branch of the Atlantic storm track during periods of NAO growth between 1960 and the mid-1990s and after 2010. In general, for the period since 1976, there has been an insignificant trend of about 0.07° latitude per decade.
REFERENCES
Agee, E.M., Trends in cyclone and anticyclone frequency and comparison with periods of warming and cooling over the Northern Hemisphere, J. Clim., 1991, vol. 4, pp. 263–267.
Bardin, M.Yu., Major modes of variability of cyclone frequency in winter in the Atlantic sector, Meteorol. Gidrol., 2000, no. 1, pp. 42–55.
Bardin, M.Yu. and Polonskii, A.B., North Atlantic Oscillation and synoptic variability in the European–Atlantic region in winter, Izv., Atmos. Ocean. Phys., 2005, vol. 41, no. 2, pp. 127–136.
Bardin, M.Yu., Platova, T.V., and Samokhina, O.F., Features of the variability of cyclonic activity in midlatitudes of the Northern Hemisphere associated with leading modes of atmospheric circulation in the Atlantic–European sector, Fundam. Prikl. Klimatol., 2015, no. 2, pp. 14–40.
Bardin, M.Yu., Platova, T.V., and Samokhina, O.F., Variability of anticyclonic activity in mid-latitudes of the Northern Hemisphere, Fundam. Prikl. Klimatol., 2019, no. 3, pp. 32–58.
Bardin, M.Yu., Ran’kova, E.Ya., Platova, T.V., Samokhina, O.F., and Korneva, I.A., Modern surface climate change as inferred from routine climate monitoring data, Russ. Meteorol. Hydrol., 2020, vol. 45, no. 5, pp. 317–329.
Barnes, E. and Polvani, L., Response of the midlatitude jets, and of their variability, to increased greenhouse gases in the CMIP5 models, J. Clim., 2013, vol. 26, pp. 7117–7135.
Barnston, A.G. and Livezey, R.E., Classification, seasonality and persistence of low-frequency atmospheric circulation patterns, Mon. Wea. Rev., 1987, vol. 115, pp. 1083–1126.
Cherenkova, E.A., Bardin, M.Yu., Platova, T.V., and Semenov, V.A., Influence of North Atlantic SST variability and changes in atmospheric circulation on the frequency of summer droughts in the East European Plain, Russ. Meteorol. Hydrol., 2020, vol. 45, no. 12, pp. 819–829.
Cornes, R.C. and Jones, P.D., An examination of storm activity in the northeast Atlantic region over the 1851–2003 period using the EMULATE gridded MSLP data series, J. Geophys. Res.: Atmos., 2011, vol. 116, p. D16110.
Deser, C., Phillips, A., Bourdette, V., and Teng, H.Y., Uncertainty in climate change projections: The role of internal variability, Clim. Dyn., 2012, vol. 38, pp. 527–546.
Diaz, H.F. and Fullbright, D.C., Eigenvector analysis of seasonal temperature, precipitation, and synoptic-scale system frequency over contiguous United States. Part 1: Winter, Mon. Weather Rev., 1981, vol. 109, pp. 1267–1284.
Gillett, N.A. and Fyfe, J.C., Annular Mode change in the CMIP5 simulations, Geophys. Res. Lett., 2013, vol. 40, pp. 1189–1193.
Gulev, S.K., Zolina, O., and Grigoriev, S., Extratropical cyclone variability in the Northern Hemisphere winter from the NCEP/NCAR Reanalysis data, Clim. Dyn., 2001, vol. 17, pp. 795–809.
IPCC, Climate Change 2013: The Physical Science, Basis., Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Stocker, T. F., Qin, D., Plattner, G.-K., et al., Eds., Cambridge: Cambridge Univ. Press, 2013.
Kalnay, E., Kanamitsu, M., Kistler, R., et al., The NCEP/NCAR 40-year reanalysis project, Bull. Am. Meteorol. Soc., 1996, vol. 77, pp. 437–470.
Kurganskaya, V.M., Conditions for the development and displacement of southern cyclones in the summer half of the year to the European territory of the USSR, Tr. Tsentr. Inst. Prognozov, 1949, no. 16, pp. 3–29.
Lau, N.C., Variability of the observed midlatitude storm tracks in relation to low-frequency changes in the circulation pattern, J. Atmos. Sci., 1988, vol. 45, pp. 2718–2743.
Lorentz, E., The Nature and Theory of the General Circulation of the Atmosphere, WMO, 1967; Leningrad: Gidrometeoizdat, 1970.
Monin, A.S., Vvedenie v teoriyu klimata (An Introduction to the Theory of Climate), Leningrad: Gidrometeoizdat, 1982.
Mul’tanovskii, B.P., Influence of atmospheric action centers on the weather of European Russia in the warm half of the year, Geofiz. Sb., 1915, no. 3, pp. 73–97.
Neu, U., Akperov, M.G., Bellenbaum, N., Benestad, R., Blender, R., Caballero, R., Cocozza, A., Dacre, H.F., Feng, Y., Fraedrich, K., Grieger, J., Gulev, S., Hanley, J., Hewson, T., Inatsu, M., et al., IMILAST—a community effort to intercompare extratropical cyclone detection and tracking algorithms: assessing method-related uncertainties, Bull. Am. Meteorol. Soc., vol. 93, pp. 529–547. https://doi.org/10.1175/BAMS-D-11-00154.1
Osborn, T.J., Simulating the winter North Atlantic Oscillation: The roles of internal variability and greenhouse gas forcing, Clim. Dyn., 2004, vol. 22, pp. 605–623.
Polonsky, A., Bardin, M., and Voskresenskaya, E., Variability of extratropical cyclonic activity in the Northern Hemisphere associated with global processes in the ocean–atmosphere system, in Cyclones: Formation, Triggers and Control, Oouchi, K. and Fudeyasu, H., Eds., Nova Science Publ., ch. 8, pp. 161–196.
Radinovic, D., Mediterranean Cyclones and Their Influence on the Weather and Climate, WMO, 1987.
Rykachev, M.A., Types of cyclone paths in Europe in 1872–1887, Zap. Akad. Nauk, 1896, vol. 3, no. 3.
Schneidereit, A., Blender, R., Fraedrich, K., and Lunkeit, F., Icelandic climate and North Atlantic cyclones in ERA-40 reanalyses, Meteorol. Z., 2007, vol. 16, pp. 17–23.
Semenov, V.A., Latif, M., Jungclaus, J.H., and Park, W., Is the observed NAO variability during the instrumental record unusual?, Geophys. Res. Lett., vol. 35, p. L11701.
Starr, V.P., Physics of Negative Viscosity Phenomena, New York: McGraw-Hill, 1968; Moscow: Mir, 1971.
Stephenson, D.B., et al. (CMIP2 Modelling Groups), North Atlantic Oscillation response to transient greenhouse gas forcing and the impact on European winter climate: A CMIP2 multi-model assessment”, Clim. Dyn., 2006, vol. 27, pp. 410–420.
Trenberth, H., Decadal atmosphere–ocean variations in the Pacific, Clim. Dyn., 1994, vol. 9, pp. 303–319.
Ulbrich, U., Pinto, J.G., Kupfer, H., Leckebusch, G.C., Spangehl, T., and Reyers, M., Changing Northern Hemisphere storm tracks in an ensemble of IPCC climate change simulations, J. Clim., 2008, vol. 21, pp. 1669–1679.
Yin, J.H., A consistent poleward shift of the storm tracks in simulations of XXI century climate, Geophys. Res. Lett., 2005, vol. 32, p. L18701. https://doi.org/10.1029/2005GL023684
Funding
This work was supported by Topic 3.2 “Monitoring the Global Climate and the Climate of the Russian Federation and Its Regions, Including the Arctic. Development and Modernization of Monitoring Technologies” of the Roshydromet research and development plan for 2020–24, approved by order no. 745 of December 31, 2019.
This work was supported by the Russian Science Foundation, project no. 19-17-00242 “Dangerous Weather and Climate Phenomena on the Territory of Russia in the Context of Global Climate Change.”
This work was supported by the R&D topic according to the Plan of Basic Scientific Research of State Academies of Sciences no. 0148-2019-0009, AAAA-A19-119022190173-2, “Climate Change and Its Consequences for the Environment and the Population Vital Activity in Russia.”
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Bardin, M.Y., Platova, T.V. & Samokhina, O.F. Long-Period Changes in the Frequency of Cyclones in the Northern Hemisphere Temperate Latitudes. Izv. Atmos. Ocean. Phys. 59 (Suppl 2), S141–S152 (2023). https://doi.org/10.1134/S0001433823140062
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DOI: https://doi.org/10.1134/S0001433823140062