Articles | Volume 34, issue 12
https://doi.org/10.5194/angeo-34-1191-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-34-1191-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Stability of solar correction for calculating ionospheric trends
Institute of Atmospheric Physics, Bocni II, 14131 Prague, Czech Republic
Dalia Burešová
Institute of Atmospheric Physics, Bocni II, 14131 Prague, Czech Republic
Daniel Kouba
Institute of Atmospheric Physics, Bocni II, 14131 Prague, Czech Republic
Peter Križan
Institute of Atmospheric Physics, Bocni II, 14131 Prague, Czech Republic
Related authors
Jaroslav Urbář and Jan Laštovička
EGUsphere, https://doi.org/10.5194/egusphere-2024-3021, https://doi.org/10.5194/egusphere-2024-3021, 2024
Short summary
Short summary
The total electron content (TEC), GNSS/GPS signal propagation and applications of GNSS/GPS signals like positioning. Here we study long-term trends in TEC. TEC trends are regionally different; they are found to be very predominantly negative; all statistically significant trends are negative. TEC trends reveal a clear wavenumber 2 longitudinal structure in low/equatorial latitudes with strong negative trends in belts 0–60° E and 180–240° E and weak trends in 90–150° E and 270–330° E.
Jan Laštovička
Atmos. Chem. Phys., 23, 5783–5800, https://doi.org/10.5194/acp-23-5783-2023, https://doi.org/10.5194/acp-23-5783-2023, 2023
Short summary
Short summary
Increasing concentration of greenhouse gases, particularly of CO2, in the atmosphere causes well-known heating of the troposphere and surface. However, the increasing concentration of CO2 also affects higher levels of the atmosphere, the stratosphere, mesosphere, thermosphere, and ionosphere, where it results in remarkable long-term trends. This article reviews significant progress in investigations of long-term trends in the mesosphere, thermosphere, and ionosphere during the period 2018–2022.
Peter Krizan, Michal Kozubek, and Jan Lastovicka
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2020-551, https://doi.org/10.5194/acp-2020-551, 2020
Publication in ACP not foreseen
Short summary
Short summary
This paper is devoted to the occurrence of discontinuities in the ozone concentration data from the selected reanalyses, because they have large impact to the results of trend studies. The discontinuity occurrence is reanalyse dependant. The discontinuities frequently occur at the middle stratosphere and in the troposphere for a certain reanalyses. According our opinion, the reanalyses data can be used in trend studies especially in the lower stratosphere.
Jan Lastovicka, Peter Krizan, and Michal Kozubek
Ann. Geophys., 36, 181–192, https://doi.org/10.5194/angeo-36-181-2018, https://doi.org/10.5194/angeo-36-181-2018, 2018
Short summary
Short summary
The longitudinal structure in geopotential heights and meridional wind is analysed for 1979–2013 in order to find its persistence and altitudinal dependence with focus on anomalous years. Substantial deviations from the average pattern are studied for Januaries – typically the second (Euro-Atlantic) peak extends to much higher altitudes than usual. The decisive role in the existence of anomalous years appears to be played by the stationary planetary wave filtering by the zonal wind pattern.
Ilya Edemskiy, Jan Lastovicka, Dalia Buresova, John Bosco Habarulema, and Ivan Nepomnyashchikh
Ann. Geophys., 36, 71–79, https://doi.org/10.5194/angeo-36-71-2018, https://doi.org/10.5194/angeo-36-71-2018, 2018
Short summary
Short summary
An unusual geomagnetic storm effect on the ionosphere in the form of localized enhancement of total electron content southward of South Africa is investigated using data from different ionosphere sounding facilities. Global ionospheric maps allow us to get the occurrence rate of such irregularities over the period of 2002–2016 and to see its correlation with solar cycle. The events we detected occur during geomagnetic storms, but not every geomagnetic storm produces such an effect.
Michal Kozubek, Peter Krizan, and Jan Lastovicka
Ann. Geophys., 35, 279–294, https://doi.org/10.5194/angeo-35-279-2017, https://doi.org/10.5194/angeo-35-279-2017, 2017
Short summary
Short summary
A study of trends in the middle stratosphere using comparisons of four main reanalyses (ERA-Interim, JRA-55, MERRA and NCEP/NCAR). We identified that all four reanalyses show very similar trends on a season or monthly basis. We also compute trends for each grid point not as a zonal mean. This approach shows detailed features in the trend studies in both hemispheres.
M. Kozubek, P. Krizan, and J. Lastovicka
Atmos. Chem. Phys., 15, 2203–2213, https://doi.org/10.5194/acp-15-2203-2015, https://doi.org/10.5194/acp-15-2203-2015, 2015
Short summary
Short summary
The main goal of this paper is to show the geographical distribution of meridional wind for several reanalyses and to analyse the wind trends in different areas. We show two areas (100°E-160°E and 140°W-80°W) where the meridional wind is as strong as zonal wind (which is normally dominant in the stratosphere). The trends of meridional wind are significant mostly at 99% level in these areas and insignificant outside. The problem with zonal averages could affect the results.
Jaroslav Urbář and Jan Laštovička
EGUsphere, https://doi.org/10.5194/egusphere-2024-3021, https://doi.org/10.5194/egusphere-2024-3021, 2024
Short summary
Short summary
The total electron content (TEC), GNSS/GPS signal propagation and applications of GNSS/GPS signals like positioning. Here we study long-term trends in TEC. TEC trends are regionally different; they are found to be very predominantly negative; all statistically significant trends are negative. TEC trends reveal a clear wavenumber 2 longitudinal structure in low/equatorial latitudes with strong negative trends in belts 0–60° E and 180–240° E and weak trends in 90–150° E and 270–330° E.
Jan Laštovička
Atmos. Chem. Phys., 23, 5783–5800, https://doi.org/10.5194/acp-23-5783-2023, https://doi.org/10.5194/acp-23-5783-2023, 2023
Short summary
Short summary
Increasing concentration of greenhouse gases, particularly of CO2, in the atmosphere causes well-known heating of the troposphere and surface. However, the increasing concentration of CO2 also affects higher levels of the atmosphere, the stratosphere, mesosphere, thermosphere, and ionosphere, where it results in remarkable long-term trends. This article reviews significant progress in investigations of long-term trends in the mesosphere, thermosphere, and ionosphere during the period 2018–2022.
Peter Krizan, Michal Kozubek, and Jan Lastovicka
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acp-2020-551, https://doi.org/10.5194/acp-2020-551, 2020
Publication in ACP not foreseen
Short summary
Short summary
This paper is devoted to the occurrence of discontinuities in the ozone concentration data from the selected reanalyses, because they have large impact to the results of trend studies. The discontinuity occurrence is reanalyse dependant. The discontinuities frequently occur at the middle stratosphere and in the troposphere for a certain reanalyses. According our opinion, the reanalyses data can be used in trend studies especially in the lower stratosphere.
Petra Koucká Knížová, Kateřina Podolská, Kateřina Potužníková, Daniel Kouba, Zbyšek Mošna, Josef Boška, and Michal Kozubek
Ann. Geophys., 38, 73–93, https://doi.org/10.5194/angeo-38-73-2020, https://doi.org/10.5194/angeo-38-73-2020, 2020
Short summary
Short summary
Severe meteorological storm Fabienne passing above central Europe was observed. Significant variations of atmospheric and ionospheric parameters were detected. Above Europe, stratospheric temperature and wind significantly changed in coincidence with frontal transition. Within ionospheric parameters, we have detected significant wave-like activity shortly after the cold front crossed the observational point. During the storm event, we have observed strong horizontal plasma flow shears.
Peter Križan
Ann. Geophys., 37, 525–533, https://doi.org/10.5194/angeo-37-525-2019, https://doi.org/10.5194/angeo-37-525-2019, 2019
Short summary
Short summary
We observe the planetary and gravity wave activity in the vertical profile of ozone at the mid-European ozonosonde stations The performance of the used detection method is satisfactory. There are differences in the following characteristics of the structure caused by the planetary and gravity wave: the annual variation, the size, and the vertical distribution. The results are influenced by the ozonosonde vertical resolution only for small and medium structures.
Jan Lastovicka, Peter Krizan, and Michal Kozubek
Ann. Geophys., 36, 181–192, https://doi.org/10.5194/angeo-36-181-2018, https://doi.org/10.5194/angeo-36-181-2018, 2018
Short summary
Short summary
The longitudinal structure in geopotential heights and meridional wind is analysed for 1979–2013 in order to find its persistence and altitudinal dependence with focus on anomalous years. Substantial deviations from the average pattern are studied for Januaries – typically the second (Euro-Atlantic) peak extends to much higher altitudes than usual. The decisive role in the existence of anomalous years appears to be played by the stationary planetary wave filtering by the zonal wind pattern.
Ilya Edemskiy, Jan Lastovicka, Dalia Buresova, John Bosco Habarulema, and Ivan Nepomnyashchikh
Ann. Geophys., 36, 71–79, https://doi.org/10.5194/angeo-36-71-2018, https://doi.org/10.5194/angeo-36-71-2018, 2018
Short summary
Short summary
An unusual geomagnetic storm effect on the ionosphere in the form of localized enhancement of total electron content southward of South Africa is investigated using data from different ionosphere sounding facilities. Global ionospheric maps allow us to get the occurrence rate of such irregularities over the period of 2002–2016 and to see its correlation with solar cycle. The events we detected occur during geomagnetic storms, but not every geomagnetic storm produces such an effect.
Michal Kozubek, Peter Krizan, and Jan Lastovicka
Ann. Geophys., 35, 279–294, https://doi.org/10.5194/angeo-35-279-2017, https://doi.org/10.5194/angeo-35-279-2017, 2017
Short summary
Short summary
A study of trends in the middle stratosphere using comparisons of four main reanalyses (ERA-Interim, JRA-55, MERRA and NCEP/NCAR). We identified that all four reanalyses show very similar trends on a season or monthly basis. We also compute trends for each grid point not as a zonal mean. This approach shows detailed features in the trend studies in both hemispheres.
M. Kozubek, P. Krizan, and J. Lastovicka
Atmos. Chem. Phys., 15, 2203–2213, https://doi.org/10.5194/acp-15-2203-2015, https://doi.org/10.5194/acp-15-2203-2015, 2015
Short summary
Short summary
The main goal of this paper is to show the geographical distribution of meridional wind for several reanalyses and to analyse the wind trends in different areas. We show two areas (100°E-160°E and 140°W-80°W) where the meridional wind is as strong as zonal wind (which is normally dominant in the stratosphere). The trends of meridional wind are significant mostly at 99% level in these areas and insignificant outside. The problem with zonal averages could affect the results.
M. Kozubek, E. Rozanov, and P. Krizan
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acpd-14-23891-2014, https://doi.org/10.5194/acpd-14-23891-2014, 2014
Revised manuscript not accepted
M. Kozubek, J. Laštovička, and P. Križan
Ann. Geophys., 32, 353–366, https://doi.org/10.5194/angeo-32-353-2014, https://doi.org/10.5194/angeo-32-353-2014, 2014
Short summary
Global climate change affects the whole atmosphere, including the thermosphere and ionosphere. Calculations of long-term trends in the ionosphere are critically dependent on solar activity correction of ionospheric input data. The main result of this study is the finding that the solar activity correction used in calculating ionospheric long-term trends is not stable, as was assumed in all previous investigations of ionospheric trends.
Global climate change affects the whole atmosphere, including the thermosphere and ionosphere....