نتایج جستجو برای: earth atmosphere

تعداد نتایج: 143613  

2011
Sara Seager

With over two dozen exoplanet atmospheres observed today, the field of exoplanet atmospheres is solidly established. The highlights of exoplanet atmosphere studies include: detection of molecular spectral features; constraints on atmospheric vertical temperature structure; detection of day-night temperature gradients; and a new numerical approach to atmosphere temperature and abundance retrieva...

Journal: :Astrobiology 2008
Hiroshi Ohmoto Bruce Runnegar Lee R Kump Marilyn L Fogel Balz Kamber Ariel D Anbar Paul L Knauth Donald R Lowe Dawn Y Sumner Yumiko Watanabe

s. Geochim. Cosmochim. Acta 72(12S). Morris, R.C. (1993) Genetic modeling for banded iron-formation of the Hamersley Group, Pilbara Craton, Western Australia. Precambrian Res. 60:243–286. Ohmoto, H. (2004) Archean atmosphere, hydrosphere, and biosphere. In The Precambrian Earth: Tempos and Events, Vol. 12, edited by P.G. Erickson, W. Alterman, D.R. Nelson, W.U. Mueller, and O. Catuneanu, Elsevi...

Journal: :Proceedings of the National Academy of Sciences of the United States of America 2006
Melissa G Trainer Alexander A Pavlov H Langley DeWitt Jose L Jimenez Christopher P McKay Owen B Toon Margaret A Tolbert

Recent exploration by the Cassini/Huygens mission has stimulated a great deal of interest in Saturn's moon, Titan. One of Titan's most captivating features is the thick organic haze layer surrounding the moon, believed to be formed from photochemistry high in the CH(4)/N(2) atmosphere. It has been suggested that a similar haze layer may have formed on the early Earth. Here we report laboratory ...

2008
M. Füllekrug

The Earth’s atmosphere is a large scale laboratory to study particles. Particles from stellar processes impinge on the top of the Earth’s atmosphere and propagate downward. Particles from discharge processes at the bottom of the atmosphere propagate upwards into near-Earth space. The acceleration of both particle populations in the Earth’s atmosphere produces electromagnetic radiation which is ...

2016
Paolo A. Sossi Mahesh Anand Franck Poitrasson

a Research School of Earth Sciences, Australian National University, Canberra 2601, ACT, Australia b School of Earth, Atmosphere and Environment, Monash University, Melbourne 3800, VIC, Australia c Department of Physical Sciences, Open University, Milton Keynes, MK76AA, UK d Department of Earth Sciences, The Natural History Museum, London, SW7 5BD, UK e Laboratoire Géosciences Environnement Tou...

2013
Colin Goldblatt Tyler D. Robinson Kevin J. Zahnle David Crisp

The atmospheres of terrestrial planets are expected to be in long-term radiation balance: an increase in the absorption of solar radiation warms the surface and troposphere, which leads to a matching increase in the emission of thermal radiation. Warming a wet planet such as Earth would make the atmosphere moist and optically thick such that only thermal radiation emitted from the upper troposp...

2004
Thomas J. Ahrens Andy H. Shen Sidao Ni

Previous calculations indicate that the Earth suffered impacts from objects up to Mars size. Such a giant impact may have produced a temporary ejecta-based ring that accreted to form the Moon. To simulate the surface waves from such events we approximated the cratering source as a buried pressurized sphere. For a 10 J impactor we calculated the resulting surface wave using the mode summation me...

2007
Stephen M. White

Space Weather is the study of the conditions in the solar wind that can affect life on the surface of the Earth, particularly the increasingly technologically sophisticated devices that are part of modern life. Solar radio observations are relevant to such phenomena because they generally originate as events in the solar atmosphere, including flares, coronal mass ejections and shocks, that prod...

1996
John Irwin

The results of a project which developed a rendering system to produce synthetic images of the Earth and its atmosphere using purely physical methods are presented. Two distinct features of this system are emphasised: (1) physically realistic models of the atmosphere’s density distribution, the spectral energy distribution of solar radiation impinging on the atmosphere and the molecular scatter...

Journal: :Philosophical transactions. Series A, Mathematical, physical, and engineering sciences 2014
G Avice B Marty

Iodine-plutonium-xenon isotope systematics have been used to re-evaluate time constraints on the early evolution of the Earth-atmosphere system and, by inference, on the Moon-forming event. Two extinct radionuclides ((129)I, T1/2=15.6 Ma and (244)Pu, T1/2=80 Ma) have produced radiogenic (129)Xe and fissiogenic (131-136)Xe, respectively, within the Earth, the related isotope fingerprints of whic...

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