메뉴 건너뛰기




Volumn 339, Issue 6115, 2013, Pages 64-67

Hydrogen-nitrogen greenhouse warming in earth's early atmosphere

Author keywords

[No Author keywords available]

Indexed keywords

HYDROGEN; NITROGEN;

EID: 84871917795     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1225759     Document Type: Article
Times cited : (200)

References (38)
  • 13
    • 84871873636 scopus 로고    scopus 로고
    • note
    • 2 CIA (30-32). This mechanism was considered and dismissed for the early Earth in (2).
  • 16
    • 84871884432 scopus 로고    scopus 로고
    • note
    • 2 causes significant cooling of the thermosphere. A final assessment of the hydrogen escape rates from Earth's early atmosphere awaits development of 3D multicomponent hydrodynamic escape models with coupled radiative transfer and chemistry.
  • 20
    • 2142803437 scopus 로고    scopus 로고
    • Materials and methods are available as supplementary materials on
    • Materials and methods are available as supplementary materials on Science Online.
    • Science Online
  • 21
    • 84871877877 scopus 로고    scopus 로고
    • note
    • CO2.
  • 23
    • 84871880707 scopus 로고    scopus 로고
    • note
    • CO2 using results from the radiative-convective model. See the supplementary materials for a definition of all terms and justification of the method.
  • 27
    • 84871900444 scopus 로고    scopus 로고
    • note
    • 3 as compared to the mixed layer, implying a decrease of biological productivity there by a similar factor (26).
  • 28
    • 84871890936 scopus 로고    scopus 로고
    • note
    • 2 inventory on a time scale on the order of 100 million years.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.