Results 101 to 110 of about 145,192 (165)

Phosphate scarcity governs methane production in the global open ocean. [PDF]

Proc Natl Acad Sci U S A
Wang S, Xu H, Weber TS.
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Gas mixing control system for the preservation of aquatic products using modified atmosphere packaging. [PDF]

Sci Rep
Lin X, Zhou L, Wang X, Zhang B, Ma S, Ding Y.   +5 more
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Deglacial stratification of the polar Southern Ocean. [PDF]

Proc Natl Acad Sci U S A
Fripiat F, Sigman DM, Ai XE, Dumoulin C, Moretti S, Studer AS, Diekmann B, Esper O, Frederichs T, Lamy F, Liu L, Pattyn F, Schmitt M, Tiedemann R, Haug GH, Martínez-García A.   +15 more
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Volcanism-induced collapse and recovery of the Atlantic meridional overturning circulation under glacial conditions. [PDF]

Sci Adv
Vettoretti G, Hu RJ, Bethke I, Krüger K, Sigl M, Outten S, Lin J, Nuterman R, Svensson A, Ditlevsen P, Jochum M.   +10 more
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The Antarctic coastal ocean heat budget is dominated by heat loss to land ice melt. [PDF]

Sci Adv
Moorman R, Thompson AF, Youngs MK, Stewart AL.   +3 more
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Spatial variation of energy transport mechanisms within solar flare ribbons. [PDF]

Nat Astron
Kerr GS, Krucker S, Allred JC, Rodríguez-Gómez JM, Inglis AR, Ryan DF, Hayes LA, Milligan RO, Kowalski AF, Plowman JE, Young PR, Kucera TA, Brosius JW.   +12 more
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Red-light photoredox catalysis with bridged fluorescein derivatives: mechanistic insights and application to fluoride-responsive photopolymerization. [PDF]

Chem Sci
Lee D, Kim H, Jung B, Yang SH, Lee HI, Lee JK.   +5 more
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Mars: Upper Atmosphere

Science, 1966
The thermal structure of the upper atmosphere of Mars has been theoretically investigated. The exospheric temperature, for a pure CO 2 model atmosphere, lies between 400° and 700°K. The origin of the Martian atmosphere is discussed in the light of these results.
S H, Gross, W E, McGovern, S I, Rasool
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Upper atmospheric nomenclature

Journal of Atmospheric and Terrestrial Physics, 1950
It is proposed that stratosphere shall signify solely the nearly isothermal region above the troposphere; that the layer between the stratosphere and the deep temperature minimum somewhat below 100 km be called the mesosphere; that the layer of rising temperature over this minimum be called the thermosphere.
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