Here we assess the evidence for the placing of magnetic and fossil biozonal boundaries in Upper T... more Here we assess the evidence for the placing of magnetic and fossil biozonal boundaries in Upper Tithonian to Lower Berriasian (Jurassic–Cretaceous boundary) sedimentary rocks on the Black Sea coast south of Theodosia (Ukraine): that is, in magnetozones M19n to M17r.
We consider our earlier-published results from these sections in relation to the correlative pattern that has become well established further west in Tethys. Additionally, this is compared and contrasted with other, alternative, results from Crimea that have been published in recent times.
This paper offers a new explanation of the observed rise of surface air temperature until the end... more This paper offers a new explanation of the observed rise of surface air temperature until the end of the 20-th century and its stabilisation after that. The temporal, as well as the diverse spatial distribution of climate change, we attribute to corresponding variations of helio- and geomagnetic fields. The mechanism of such an influence consists of modulation the intensity, and depth of penetration into the Earth’s atmosphere, of highly energetic particles with galactic and solar origin. Releasing their energy at different altitudes, these particles activate ion-molecular reactions of different types, which impact the ozone balance in the lower stratosphere. The latter controls the temperature and humidity near the tropopause − through an influence on the atmospheric static stability. The highest impact of the upper tropospheric water vapour in the Earth’s radiation budget mediates the ozone influence down to the surface, through strengthening or weakening of the greenhouse effect. Thus O3 abundance near the tropopause reduces humidity and cools the Earth’s surface air temperature, while ozone depletion – cools it.
Here we assess the evidence for the placing of magnetic and fossil biozonal boundaries in Upper T... more Here we assess the evidence for the placing of magnetic and fossil biozonal boundaries in Upper Tithonian to Lower Berriasian (Jurassic–Cretaceous boundary) sedimentary rocks on the Black Sea coast south of Theodosia (Ukraine): that is, in magnetozones M19n to M17r.
We consider our earlier-published results from these sections in relation to the correlative pattern that has become well established further west in Tethys. Additionally, this is compared and contrasted with other, alternative, results from Crimea that have been published in recent times.
This paper offers a new explanation of the observed rise of surface air temperature until the end... more This paper offers a new explanation of the observed rise of surface air temperature until the end of the 20-th century and its stabilisation after that. The temporal, as well as the diverse spatial distribution of climate change, we attribute to corresponding variations of helio- and geomagnetic fields. The mechanism of such an influence consists of modulation the intensity, and depth of penetration into the Earth’s atmosphere, of highly energetic particles with galactic and solar origin. Releasing their energy at different altitudes, these particles activate ion-molecular reactions of different types, which impact the ozone balance in the lower stratosphere. The latter controls the temperature and humidity near the tropopause − through an influence on the atmospheric static stability. The highest impact of the upper tropospheric water vapour in the Earth’s radiation budget mediates the ozone influence down to the surface, through strengthening or weakening of the greenhouse effect. Thus O3 abundance near the tropopause reduces humidity and cools the Earth’s surface air temperature, while ozone depletion – cools it.
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Papers by V.G. Bakhmuto
We consider our earlier-published results from these sections in relation to the correlative pattern that has become well established further west in Tethys. Additionally, this is compared and contrasted with other, alternative, results from Crimea that have been published in recent times.
spatial distribution of climate change, we attribute to corresponding variations of helio- and geomagnetic fields. The mechanism of such an influence consists of modulation the intensity, and depth of penetration into the Earth’s atmosphere, of highly energetic particles with galactic and solar origin. Releasing their energy at different altitudes, these particles activate ion-molecular reactions of different types, which impact the ozone balance in the lower stratosphere. The latter controls the temperature and humidity near the tropopause − through an influence on the atmospheric static stability. The highest impact of the upper
tropospheric water vapour in the Earth’s radiation budget mediates the ozone influence down to the surface, through strengthening or weakening of the greenhouse effect. Thus O3 abundance near the tropopause reduces humidity and cools the Earth’s surface air temperature, while ozone depletion – cools it.
We consider our earlier-published results from these sections in relation to the correlative pattern that has become well established further west in Tethys. Additionally, this is compared and contrasted with other, alternative, results from Crimea that have been published in recent times.
spatial distribution of climate change, we attribute to corresponding variations of helio- and geomagnetic fields. The mechanism of such an influence consists of modulation the intensity, and depth of penetration into the Earth’s atmosphere, of highly energetic particles with galactic and solar origin. Releasing their energy at different altitudes, these particles activate ion-molecular reactions of different types, which impact the ozone balance in the lower stratosphere. The latter controls the temperature and humidity near the tropopause − through an influence on the atmospheric static stability. The highest impact of the upper
tropospheric water vapour in the Earth’s radiation budget mediates the ozone influence down to the surface, through strengthening or weakening of the greenhouse effect. Thus O3 abundance near the tropopause reduces humidity and cools the Earth’s surface air temperature, while ozone depletion – cools it.