[Relationship between ozon changes and solar variability through climate observation]

English. A number of photo model studies of the earth's atmosphere have raised the possibility that atmospheric O3 concentrations may be altered significantly by antropogenic sources of trace chemical species and by solar variability. The possible climatic effect of such O3, parturbations, as they are understood currently, are reviewed. A change in tropospheric O3 can influence the tropospheric climate directly through its effect on tropospheric radiative heating, where as stratospheric O3 change exerts its influence on the tropospheric climate through radiative and dynamical coupling mechanics. Changes in both tropospheric and stratospheric O3 are considered and model result are described for their effects on: surface temperature, surface tropospheric radiative heating, and vertical and latitudinal temperature gradients within the stratospheric. The solar variability effects on stratospheric temperature gradients and on radiative dissipation rates are discussed

unknown. Sejumlah studi foto kimia atmosfer bumi telah menyimpulkan suatu kemungkinan bahwa konsentrasi ozon-O3 diubah oleh sumber antropogenic dari jenis bahan kimia dan oleh variabilitas matahari. Kemungkinan iklim dipengaruhi oleh gangguan ozon, pada waktu ini telah diketahui. Perubahan ozon di troposfer dapat mempengaruhi iklim di troposfer secara langsung melalui pengaruh pemanasan radiasi pada troposfer, dimana perubahan ozon di stratosfer mempengaruhi iklim troposfer melalui radiasi dan gabungan dinamika. Perubahan ozon di troposfer dan di stratosfer telah diteliti dan menghasilkan model, pengaruhnya pada: temperatur permukaan, pemanasan radiasi pada permukaan troposfer dan temperatur gradient arah vertikal dan lintang di daerah stratosfer. Pengaruh variabilitas matahari pada temperatur gradien di stratosfer dan kecepatan menghamburnya radiasi akan dibahas