LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY
Subject and Purpose. The troposphere is a natural channel for the propagation of meter- and shorter wavelength radio waves. Studying the impact of solar activity (SA) on the condition of the troposphere is important for improving the accuracy of weather forecasts and understanding the state of the t...
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Zakharov, I. G. Chernogor, L. F. LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
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сонячна активність 27-денний цикл стратосферно-тропосферна взаємодія |
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Article |
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Zakharov, I. G. Chernogor, L. F. |
| author_facet |
Zakharov, I. G. Chernogor, L. F. |
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Zakharov, I. G. |
| title |
LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
| title_short |
LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
| title_full |
LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
| title_fullStr |
LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
| title_full_unstemmed |
LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY |
| title_sort |
latitudinal features of tropospheric response to 27-day cyclic variations of solar activity |
| title_alt |
ШИРОТНІ ОСОБЛИВОСТІ ВІДГУКУ ТРОПОСФЕРИ НА 27-ДЕННІ КОЛИВАННЯ СОНЯЧНОЇ АКТИВНОСТІ |
| description |
Subject and Purpose. The troposphere is a natural channel for the propagation of meter- and shorter wavelength radio waves. Studying the impact of solar activity (SA) on the condition of the troposphere is important for improving the accuracy of weather forecasts and understanding the state of the tropospheric radio channel. The present paper has been aimed at identifying and comprehending the solar-tropospheric interactions resulting from the 27-day cycles of solar activity.Methods and Methodology.The study was conducted through twenty 27-day cycles of solar activity, over an interval of latitudes between 0 and 80°N, and at four east longitudes, specifically 30, 180, 240 and 330°E. The atmospheric data used were quoted from the NOAA Physical Sciences Laboratory list (https://psl.noaa.gov /data/timeseries/daily/) and concerned sea level pressure, temperature in the troposphere at the height level with a 1000 hPa pressure, stratospheric temperature at the height corresponding to 50 hPa, and zonal wind speed.Results. Reliable estimates have been obtained for the atmospheric parameters varying over 27-day cycles, that revealed maximum amplitudes at middle and high latitudes,: in particular the sea level pressure up to 12 hPa, temperature in the troposphere up to 5.3 K, and up to 3.5 K in the stratosphere . The relative amplitudes (about 1.3%) of these variations correlate with the 27-day changes in the solar UV radiation of a 205 nm wavelength. Anti-phase changes have been observed between the troposphere and stratosphere temperatures over the continents in the Western and Eastern hemispheres, as well as anti-phase changes in pressure over the continentsand the oceans. The change in the sign of temperature variation with height occurs near the tropopause, being accompanied by a ~ 1 km change in the tropopause height. At the latitude of 60°N, the 27-day changes in the zonal wind speed in the stratosphere may reach tens per cent. A persistent solar effect is observable not in winter time alone, but in summer as well, while of a smaller amplitude.Conclusions. Owing to stratosphere-troposphere interaction effects, the troposphere demonstrates a high sensitivity to 27-day variations of the solar UV radiation. The main properties of the 27-day variations of atmospheric parameters testify to the importantrole of planetary and meteorological- scale Rossby waves in the realization of solar influence.Keywords: solar activity; 27-day cycle; stratosphere-troposphere interactionsManuscript submitted 25.03.2024Radio phys. radio astron. 2024, 29(4): 293-307REFERENCES1. Dikty, S., Weber, M., von Savigny, C., Sonkaew, T., Rozanov, A., Burrows, J.P., 2010. Modulations of the 27 day solar rotation signal in stratospheric ozone from Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) (2003—2008). J. Geophys. Res., 115(D1). DOI: https://doi.org/10.1029/2009JD0123792. Fioletov, V.E., 2009. Estimating the 27‐day and 11‐year solar cycle variations in tropical upper stratospheric ozone. J. Geophys. Res., 114(D2). DOI: https://doi.org/10.1029/2008JD0104993. Gruzdev, A.N., Schmidt, H., Brasseur, G.P., 2009. The effect of the solar rotational irradiance variation on the middle and upper atmosphere calculated by a three‐dimensional chemistry‐climate model. Atmos. Chem. Phys., 8, pp. 1113—1158. DOI: https://doi.org/10.5194/acpd-8-1113-20084. Hood, L.L., Zhou, S., 1998. Stratospheric effects of 27-day solar ultraviolet variations: An analysis of UARS MLS ozone and temperature data. J. Geophys. Res., 103(D3), pp. 3629—3638. DOI: https://doi.org/10.1029/97JD028495. Kubin, A., Langematz, U., Brühl, C., 2011. Chemistry climate model simulations of the effect of the 27 day solar rotational cycle on ozone. J. Geophys. Res., 116(D15). DOI: https://doi.org/10.1029/2011JD0156656. Ruzmaikin, A., Santee, M.L., Schwartz, M.J., Froidevaux, L., Pickett, H.M., 2007. The 27‐day variations in stratospheric ozone and temperature: New MLS data. Geophys. Res. Lett., 34(2). DOI: https://doi.org/10.1029/2006GL0284197. Burns, G.B., Tinsley, B.A., French, W.J.R., Troshichev, O.A., Frank-Kamenetsky, A.V., 2008. Atmospheric circuit influences on ground-level pressure in the Antarctic and Arctic. J. Geophys. Res. Atmos., 113(D15). DOI: https://doi.org/10.1029/2007JD0096188. Edmonds, I., 2013. The correlation of ~ 27 day period solar activity and daily maximum temperature in continental Australia. 2013. arXiv:1307.0921 [astro-ph.SR]. DOI: 10.48550/arXiv.1307.09219. Hood, L.L., 2003. Thermal response of the tropical tropopause region to solar ultraviolet variations. Geophys. Res. Lett., 30(23). DOI: https://doi.org/10.1029/2003GL01836410. Takahashi, Y., Okazaki, Y., Sato, M., Miyahara, H. Sakanoi, K., Hong, P.K., Hoshino, N., 2010. 27-day variation in cloud amount in the Western pacific warm pool region and relationship to the solar cycle. Atmos. Chem. Phys., 10, pp. 1577—1584. DOI: https://doi.org/10.5194/acp-10-1577-201011. Gray, L.J., Beer, J., Geller, M., Haigh, J.D., Lockwood, M., Matthes, K., Cubasch, U., Fleitmann, D., Harrison, G., Hood, L., Luterbacher, J., Meehl, G.A., Shindell, D., van Geel, B., White, W., 2010. Solar influences on climate. Rev. Geophys., 48(4). DOI: https://doi.org/10.1029/2009RG00028212. Protsenko, G.D., 2007. Meteorology and climatology. Kyiv, Dragomanov Ukrainian State University Publ. (in Ukrainian).13. Ashok, K., Behera, S.K., Rao, S.A., Weng, H., Yamagata, T., 2007. El Niño Modoki and its possible teleconnection. J. Geophys. Res., 112(C11). DOI: https://doi.org/10.1029/2006JC00379814. Evtushevsky, O.M., Kravchenko, V.O., Hood, L.L, Milinevsky, G.P., 2015. Teleconnection between the central tropical Pacific and the Antarctic stratosphere: spatial patterns and time lags. Clim. Dyn., 44, pp. 1841—1855. DOI: https://doi.org/10.1007/s00382-014-2375-215. Wallace, J.M., Gutzler, D.S., 1981. Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon. Weather Rev., 109, pp. 784—812. DOI: https://doi.org/10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;216. Wirth, V., Riemer, M., Chang, E.K., Martius, O., 2018. Rossby Wave Packets on the Midlatitude Waveguide. Mon. Weather Rev., 146(7), pp. 1965—2001. DOI: https://doi.org/10.1175/MWR-D-16-0483.117. Shepherd, T.G., 2002. Issues in stratosphere–troposphere coupling. J. Meteorol. Soc. Japan., 80(4B), pp. 769—792.DOI: https://doi.org/10.2151/jmsj.80.76918. Charney, J.G., Drazin, P.G., 1961. Propagation of planetary-scale disturbances from the lower into the upper atmosphere. J. Geophys. Res., 66, pp. 83—109. DOI: https://doi.org/10.1029/JZ066i001p0008319. Canziani, P.O., Legnani, W.E., 2003. Tropospheric–stratospheric coupling: Extratropical synoptic systems in the lower stratosphere. Part A. Q. J. R. Meteorolog. Soc., 129(592), pp. 2315—2329. DOI: https://doi.org/10.1256/qj.01.10920. Colucci, S.J., 2010. Stratospheric influences on tropospheric weather systems. J. Atmos. Sci., 67(2), pp. 324—344. DOI:https://doi.org/10.1175/2009JAS3148.121. Baldwin, M.P., Ayarzagüena, B., Birner, T., Butchart, N., Butler, A.H., Charlton-Perez, A.J., Domeisen, D.I.V., Garfinkel, C.I., Garny, H., Gerber, E.P., Hegglin, M.I., Langematz, U., Pedatella, N.M., 2021. Sudden stratospheric warmings. Rev. Geophys., 59(1).DOI: https://doi.org/10.1029/2020RG00070822. Butchart, N., 2014. The Brewer-Dobson circulation. Rev. Geophys., 52, pp. 157—184. DOI: https://doi.org/10.1002/2013RG00044823. Dunn-Sigouin, E., Shaw, T.A., 2015. Comparing and contrasting extreme stratospheric events, including their coupling to the tropospheric circulation. J. Geophys. Res., 120(4), pp. 1374—1391. DOI: https://doi.org/10.1002/2014JD02211624. Kidston, J., Scaife, A.A., Hardiman, S.C., Mitchell, D.M., Butchart, N., Baldwin, M.P., Gray, L.J., 2015. Stratospheric infl uence on tropospheric jet streams, storm tracks and surface weather. Nat. Geosci., 8(6), pp. 433—440. DOI: https://doi.org/10.1038/ngeo242425. Milinevsky, G.P., Grytsai, A.V., Evtushevsky, O.M., Klekociuk, A.R., 2022. Contributions to understanding climate interactions: stratospheric ozone. Kyiv: Akademperiodyka Publ. DOI: https://doi.org/10.15407/academperiodyka.252.47126. Mitchell, D.M., Gray, L.J., Anstey, J., Baldwin, M.P., Charlton-Perez, A.J., 2013. The infl uence of stratospheric vortex displacements and splits on surface climate. J. Clim., 26(8), pp. 2668—2682. DOI: https://doi.org/10.1175/JCLI-D-12-00030.127. Shaw, T.A., Perlwitz, J., Weiner, O., 2014. Troposphere–stratosphere coupling: Links to North Atlantic weather and climate, including their representation in CMIP5 models. J. Geophys. Res., 119(10), pp. 5864—5880. DOI: https://doi.org/10.1002/2013JD02119128. Kodera, K., Kuroda, Y., 2002. Dynamical response to the solar cycle. J. Geopys. Res., 107(D24). DOI: https://doi.org/10.1029/2002JD00222429. Williams, G.P., 2006. Circulation sensitivity to tropopause height. J. Atmos. Sci., 63(7), pp. 1954—1961. DOI: https://doi.org/10.1175/JAS3762.130. Kashkin, V.B., 2014. Internal gravity waves in the troposphere. Atmos. Oceanic Opt., 27, pp. 1—9. DOI: https://doi.org/10.1134/S102485601401005931. Daocheng, Yu, Xiaohua, Xu, Jia, Luo, Juan, Li., 2019. On the relationship between gravity waves and tropopause height and temperature over the globe revealed by COSMIC radio occultation measurements. Atmosphere, 10(75). DOI: https://doi.org/10.3390/atmos1002007532. Boljka, L., Birner, T., 2020. Tropopause-level planetary wave source and its role in two-way troposphere–stratosphere coupling. Weather Clim. Dyn., 1, pp. 555—575. DOI: https://doi.org/10.5194/wcd-1-555-202033. Boljka, L., Birner, T., 2022. Potential impact of tropopause sharpness on the structure and strength of the general circulation. NPJ Clim. Atmos. Sci., 5(98). DOI: https://doi.org/10.1038/s41612-022-00319-634. Karen, L., Smith, R., Scott, K., 2016. The role of planetary waves in the tropospheric jet response to stratospheric cooling. Geophys. Res. Lett., 43(6), pp. 2904—2911. DOI: https://doi.org/10.1002/2016GL06784935. Putz, C., Schlutow, M., Klein, R., Bense, V., Spichtinger, P., 2018. Reflection and transmission of gravity waves at non-uniform stratification layers. arXiv: 1812.08779v1[physics.ao-ph]. DOI: 10.48550/arXiv.1812.0877936. Stone, K.A., Solomon, S., Kinnison, D.E., Baggett, C.F., Barnes, E.A., 2019. Prediction of Northern Hemisphere regional surface temperatures using stratospheric ozone information. J. Geoph. Res. Atmos., 124(12). DOI: https://doi.org/10.1029/2018JD02962637. Yang, S.-S., Pan, C.-J., Das, U., 2021. Investigating the spatio-temporal distribution of gravity wave potential energy over the equatorial region using the ERA5 reanalysis data. Atmosphere, 12(311). DOI: https://doi.org/10.3390/atmos1203031138. Song, Y., Robinson, W.A., 2004. Dynamical mechanisms for stratospheric influences on the troposphere. J. Atmos. Sci., 61(14), pp. 1711—1725. DOI: https://doi.org/10.1175/1520-0469(2004)061<1711:DMFSIO>2.0.CO;239. Lee, J.N., Hameed, S., Shindell, D.T., 2008. Northern annular mode in summer and its relation to solar activity variations in the GISS Model E. J. Atmos. Sol. Terr. Phys., 70(5), pp. 730—741. DOI: https://doi.org/10.1016/j.jastp.2007.10.012 |
| publisher |
Видавничий дім «Академперіодика» |
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2024 |
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http://rpra-journal.org.ua/index.php/ra/article/view/1455 |
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rpra-journalorgua-article-14552024-12-17T08:35:29Z LATITUDINAL FEATURES OF TROPOSPHERIC RESPONSE TO 27-DAY CYCLIC VARIATIONS OF SOLAR ACTIVITY ШИРОТНІ ОСОБЛИВОСТІ ВІДГУКУ ТРОПОСФЕРИ НА 27-ДЕННІ КОЛИВАННЯ СОНЯЧНОЇ АКТИВНОСТІ Zakharov, I. G. Chernogor, L. F. сонячна активність; 27-денний цикл; стратосферно-тропосферна взаємодія Subject and Purpose. The troposphere is a natural channel for the propagation of meter- and shorter wavelength radio waves. Studying the impact of solar activity (SA) on the condition of the troposphere is important for improving the accuracy of weather forecasts and understanding the state of the tropospheric radio channel. The present paper has been aimed at identifying and comprehending the solar-tropospheric interactions resulting from the 27-day cycles of solar activity.Methods and Methodology.The study was conducted through twenty 27-day cycles of solar activity, over an interval of latitudes between 0 and 80°N, and at four east longitudes, specifically 30, 180, 240 and 330°E. The atmospheric data used were quoted from the NOAA Physical Sciences Laboratory list (https://psl.noaa.gov /data/timeseries/daily/) and concerned sea level pressure, temperature in the troposphere at the height level with a 1000 hPa pressure, stratospheric temperature at the height corresponding to 50 hPa, and zonal wind speed.Results. Reliable estimates have been obtained for the atmospheric parameters varying over 27-day cycles, that revealed maximum amplitudes at middle and high latitudes,: in particular the sea level pressure up to 12 hPa, temperature in the troposphere up to 5.3 K, and up to 3.5 K in the stratosphere . The relative amplitudes (about 1.3%) of these variations correlate with the 27-day changes in the solar UV radiation of a 205 nm wavelength. Anti-phase changes have been observed between the troposphere and stratosphere temperatures over the continents in the Western and Eastern hemispheres, as well as anti-phase changes in pressure over the continentsand the oceans. The change in the sign of temperature variation with height occurs near the tropopause, being accompanied by a ~ 1 km change in the tropopause height. At the latitude of 60°N, the 27-day changes in the zonal wind speed in the stratosphere may reach tens per cent. A persistent solar effect is observable not in winter time alone, but in summer as well, while of a smaller amplitude.Conclusions. Owing to stratosphere-troposphere interaction effects, the troposphere demonstrates a high sensitivity to 27-day variations of the solar UV radiation. The main properties of the 27-day variations of atmospheric parameters testify to the importantrole of planetary and meteorological- scale Rossby waves in the realization of solar influence.Keywords: solar activity; 27-day cycle; stratosphere-troposphere interactionsManuscript submitted 25.03.2024Radio phys. radio astron. 2024, 29(4): 293-307REFERENCES1. Dikty, S., Weber, M., von Savigny, C., Sonkaew, T., Rozanov, A., Burrows, J.P., 2010. Modulations of the 27 day solar rotation signal in stratospheric ozone from Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) (2003—2008). J. Geophys. Res., 115(D1). DOI: https://doi.org/10.1029/2009JD0123792. Fioletov, V.E., 2009. Estimating the 27‐day and 11‐year solar cycle variations in tropical upper stratospheric ozone. J. Geophys. Res., 114(D2). DOI: https://doi.org/10.1029/2008JD0104993. Gruzdev, A.N., Schmidt, H., Brasseur, G.P., 2009. The effect of the solar rotational irradiance variation on the middle and upper atmosphere calculated by a three‐dimensional chemistry‐climate model. Atmos. Chem. Phys., 8, pp. 1113—1158. DOI: https://doi.org/10.5194/acpd-8-1113-20084. Hood, L.L., Zhou, S., 1998. Stratospheric effects of 27-day solar ultraviolet variations: An analysis of UARS MLS ozone and temperature data. J. Geophys. Res., 103(D3), pp. 3629—3638. DOI: https://doi.org/10.1029/97JD028495. Kubin, A., Langematz, U., Brühl, C., 2011. Chemistry climate model simulations of the effect of the 27 day solar rotational cycle on ozone. J. Geophys. Res., 116(D15). DOI: https://doi.org/10.1029/2011JD0156656. Ruzmaikin, A., Santee, M.L., Schwartz, M.J., Froidevaux, L., Pickett, H.M., 2007. The 27‐day variations in stratospheric ozone and temperature: New MLS data. Geophys. Res. Lett., 34(2). DOI: https://doi.org/10.1029/2006GL0284197. Burns, G.B., Tinsley, B.A., French, W.J.R., Troshichev, O.A., Frank-Kamenetsky, A.V., 2008. Atmospheric circuit influences on ground-level pressure in the Antarctic and Arctic. J. Geophys. Res. Atmos., 113(D15). DOI: https://doi.org/10.1029/2007JD0096188. Edmonds, I., 2013. The correlation of ~ 27 day period solar activity and daily maximum temperature in continental Australia. 2013. arXiv:1307.0921 [astro-ph.SR]. DOI: 10.48550/arXiv.1307.09219. Hood, L.L., 2003. Thermal response of the tropical tropopause region to solar ultraviolet variations. Geophys. Res. Lett., 30(23). DOI: https://doi.org/10.1029/2003GL01836410. Takahashi, Y., Okazaki, Y., Sato, M., Miyahara, H. Sakanoi, K., Hong, P.K., Hoshino, N., 2010. 27-day variation in cloud amount in the Western pacific warm pool region and relationship to the solar cycle. Atmos. Chem. Phys., 10, pp. 1577—1584. DOI: https://doi.org/10.5194/acp-10-1577-201011. Gray, L.J., Beer, J., Geller, M., Haigh, J.D., Lockwood, M., Matthes, K., Cubasch, U., Fleitmann, D., Harrison, G., Hood, L., Luterbacher, J., Meehl, G.A., Shindell, D., van Geel, B., White, W., 2010. Solar influences on climate. Rev. Geophys., 48(4). DOI: https://doi.org/10.1029/2009RG00028212. Protsenko, G.D., 2007. Meteorology and climatology. Kyiv, Dragomanov Ukrainian State University Publ. (in Ukrainian).13. Ashok, K., Behera, S.K., Rao, S.A., Weng, H., Yamagata, T., 2007. El Niño Modoki and its possible teleconnection. J. Geophys. Res., 112(C11). DOI: https://doi.org/10.1029/2006JC00379814. Evtushevsky, O.M., Kravchenko, V.O., Hood, L.L, Milinevsky, G.P., 2015. Teleconnection between the central tropical Pacific and the Antarctic stratosphere: spatial patterns and time lags. Clim. Dyn., 44, pp. 1841—1855. DOI: https://doi.org/10.1007/s00382-014-2375-215. Wallace, J.M., Gutzler, D.S., 1981. Teleconnections in the geopotential height field during the Northern Hemisphere winter. Mon. Weather Rev., 109, pp. 784—812. DOI: https://doi.org/10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;216. Wirth, V., Riemer, M., Chang, E.K., Martius, O., 2018. Rossby Wave Packets on the Midlatitude Waveguide. Mon. Weather Rev., 146(7), pp. 1965—2001. DOI: https://doi.org/10.1175/MWR-D-16-0483.117. Shepherd, T.G., 2002. Issues in stratosphere–troposphere coupling. J. Meteorol. Soc. Japan., 80(4B), pp. 769—792.DOI: https://doi.org/10.2151/jmsj.80.76918. Charney, J.G., Drazin, P.G., 1961. Propagation of planetary-scale disturbances from the lower into the upper atmosphere. J. Geophys. Res., 66, pp. 83—109. DOI: https://doi.org/10.1029/JZ066i001p0008319. Canziani, P.O., Legnani, W.E., 2003. Tropospheric–stratospheric coupling: Extratropical synoptic systems in the lower stratosphere. Part A. Q. J. R. Meteorolog. Soc., 129(592), pp. 2315—2329. DOI: https://doi.org/10.1256/qj.01.10920. Colucci, S.J., 2010. Stratospheric influences on tropospheric weather systems. J. Atmos. Sci., 67(2), pp. 324—344. DOI:https://doi.org/10.1175/2009JAS3148.121. Baldwin, M.P., Ayarzagüena, B., Birner, T., Butchart, N., Butler, A.H., Charlton-Perez, A.J., Domeisen, D.I.V., Garfinkel, C.I., Garny, H., Gerber, E.P., Hegglin, M.I., Langematz, U., Pedatella, N.M., 2021. Sudden stratospheric warmings. Rev. Geophys., 59(1).DOI: https://doi.org/10.1029/2020RG00070822. Butchart, N., 2014. The Brewer-Dobson circulation. Rev. Geophys., 52, pp. 157—184. DOI: https://doi.org/10.1002/2013RG00044823. Dunn-Sigouin, E., Shaw, T.A., 2015. Comparing and contrasting extreme stratospheric events, including their coupling to the tropospheric circulation. J. Geophys. Res., 120(4), pp. 1374—1391. DOI: https://doi.org/10.1002/2014JD02211624. Kidston, J., Scaife, A.A., Hardiman, S.C., Mitchell, D.M., Butchart, N., Baldwin, M.P., Gray, L.J., 2015. Stratospheric infl uence on tropospheric jet streams, storm tracks and surface weather. Nat. Geosci., 8(6), pp. 433—440. DOI: https://doi.org/10.1038/ngeo242425. Milinevsky, G.P., Grytsai, A.V., Evtushevsky, O.M., Klekociuk, A.R., 2022. Contributions to understanding climate interactions: stratospheric ozone. Kyiv: Akademperiodyka Publ. DOI: https://doi.org/10.15407/academperiodyka.252.47126. Mitchell, D.M., Gray, L.J., Anstey, J., Baldwin, M.P., Charlton-Perez, A.J., 2013. The infl uence of stratospheric vortex displacements and splits on surface climate. J. Clim., 26(8), pp. 2668—2682. DOI: https://doi.org/10.1175/JCLI-D-12-00030.127. Shaw, T.A., Perlwitz, J., Weiner, O., 2014. Troposphere–stratosphere coupling: Links to North Atlantic weather and climate, including their representation in CMIP5 models. J. Geophys. Res., 119(10), pp. 5864—5880. DOI: https://doi.org/10.1002/2013JD02119128. Kodera, K., Kuroda, Y., 2002. Dynamical response to the solar cycle. J. Geopys. Res., 107(D24). DOI: https://doi.org/10.1029/2002JD00222429. Williams, G.P., 2006. Circulation sensitivity to tropopause height. J. Atmos. Sci., 63(7), pp. 1954—1961. DOI: https://doi.org/10.1175/JAS3762.130. Kashkin, V.B., 2014. Internal gravity waves in the troposphere. Atmos. Oceanic Opt., 27, pp. 1—9. DOI: https://doi.org/10.1134/S102485601401005931. Daocheng, Yu, Xiaohua, Xu, Jia, Luo, Juan, Li., 2019. On the relationship between gravity waves and tropopause height and temperature over the globe revealed by COSMIC radio occultation measurements. Atmosphere, 10(75). DOI: https://doi.org/10.3390/atmos1002007532. Boljka, L., Birner, T., 2020. Tropopause-level planetary wave source and its role in two-way troposphere–stratosphere coupling. Weather Clim. Dyn., 1, pp. 555—575. DOI: https://doi.org/10.5194/wcd-1-555-202033. Boljka, L., Birner, T., 2022. Potential impact of tropopause sharpness on the structure and strength of the general circulation. NPJ Clim. Atmos. Sci., 5(98). DOI: https://doi.org/10.1038/s41612-022-00319-634. Karen, L., Smith, R., Scott, K., 2016. The role of planetary waves in the tropospheric jet response to stratospheric cooling. Geophys. Res. Lett., 43(6), pp. 2904—2911. DOI: https://doi.org/10.1002/2016GL06784935. Putz, C., Schlutow, M., Klein, R., Bense, V., Spichtinger, P., 2018. Reflection and transmission of gravity waves at non-uniform stratification layers. arXiv: 1812.08779v1[physics.ao-ph]. DOI: 10.48550/arXiv.1812.0877936. Stone, K.A., Solomon, S., Kinnison, D.E., Baggett, C.F., Barnes, E.A., 2019. Prediction of Northern Hemisphere regional surface temperatures using stratospheric ozone information. J. Geoph. Res. Atmos., 124(12). DOI: https://doi.org/10.1029/2018JD02962637. Yang, S.-S., Pan, C.-J., Das, U., 2021. Investigating the spatio-temporal distribution of gravity wave potential energy over the equatorial region using the ERA5 reanalysis data. Atmosphere, 12(311). DOI: https://doi.org/10.3390/atmos1203031138. Song, Y., Robinson, W.A., 2004. Dynamical mechanisms for stratospheric influences on the troposphere. J. Atmos. Sci., 61(14), pp. 1711—1725. DOI: https://doi.org/10.1175/1520-0469(2004)061<1711:DMFSIO>2.0.CO;239. Lee, J.N., Hameed, S., Shindell, D.T., 2008. Northern annular mode in summer and its relation to solar activity variations in the GISS Model E. J. Atmos. Sol. Terr. Phys., 70(5), pp. 730—741. DOI: https://doi.org/10.1016/j.jastp.2007.10.012 Предмет і мета роботи. Тропосфера є природним каналом поширення метрових і більш коротких радіохвиль. Вивчення впливу сонячної активності (СА) на тропосферу важливе для підвищення точності прогнозів погоди та стану тропосферного радіоканалу. Метою роботи є виявлення та дослідження сонячно-тропосферних зв’язків на основі 27-денних циклів СА.Методи та методологія. Дослідження проведено для двадцяти 27-денних циклів СА в інтервалі широт 0...80°N на чотирьох довготах: 30, 180, 240 та 330°E. Використано дані NOAA Physical Sciences Laboratory про атмосферний тиск на рівні моря, тропосферну температуру на рівні 1000 гПа, стратосферну температуру на рівні 50 гПа та швидкість зонального вітру (https://psl.noaa.gov/data/timeseries/daily/).Результати. Виявлено достовірні 27-денні зміни атмосферних параметрів з максимальною амплітудою на середніх і високих широтах: тиск – до 12 гПа, температура у тропосфері — до 5.3 К, у стратосфері — до 3.5 К. Відносні амплітуди цих змін відповідають 27-денним змінам сонячного УФ-випромінювання з довжиною хвилі 205 нм (1.3 %). Спостерігаються протифазні зміни температури у тропосфері та стратосфері над континентами у західній і східній півкулях та протифазні зміни тиску над континентами й океанами. Зміна знака коливань температури з висотою відбувається поблизу тропопаузи з одночасною зміною висоти тропопаузи на ~ 1 км. У стратосфері на широті 60°N 27-денні коливання швидкості зонального вітру сягають десятків відсотків. Стійкий сонячний ефект спостерігається не лише взимку, але й влітку, хоча і з меншою амплітудою.Висновки. Тропосфера, завдяки стратосферно-тропосферної взаємодії, демонструє високу чутливість до 27-денних змін сонячного УФ-випромінювання. Властивості 27-денних коливань атмосферних параметрів свідчать про важливу роль хвиль Россбі планетарного та метеорологічного масштабу у реалізації сонячного впливу.Ключові слова: сонячна активність, 27-денний цикл, стратосферно-тропосферна взаємодіяСтаття надійшла до редакції 25.12.2023Radio phys. radio astron. 2024, 29(4): 293-307БІБЛІОГРАФІЧНИЙ СПИСОК1. Dikty S., Weber M., von Savigny C., Sonkaew T., Rozanov A., Burrows J.P. Modulations of the 27 day solar rotation signal in stratospheric ozone from Scanning Imaging Absorption Spectrometer for Atmospheric Cartography (SCIAMACHY) (2003—2008). J. Geophys. Res. 2010. Vol. 115, Iss. D1. DOI: 10.1029/2009JD0123792. Fioletov V.E. 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Phys. 2008. Vol. 70, Iss. 5. P. 730—741. DOI: 10.1016/j.jastp.2007.10.012 Видавничий дім «Академперіодика» 2024-12-10 Article Article application/pdf http://rpra-journal.org.ua/index.php/ra/article/view/1455 10.15407/rpra29.04.293 РАДИОФИЗИКА И РАДИОАСТРОНОМИЯ; Vol 29, No 4 (2024); 293 RADIO PHYSICS AND RADIO ASTRONOMY; Vol 29, No 4 (2024); 293 РАДІОФІЗИКА І РАДІОАСТРОНОМІЯ; Vol 29, No 4 (2024); 293 2415-7007 1027-9636 10.15407/rpra29.04 uk http://rpra-journal.org.ua/index.php/ra/article/view/1455/pdf Copyright (c) 2024 RADIO PHYSICS AND RADIO ASTRONOMY |