메뉴 건너뛰기




Volumn 89, Issue 2, 2002, Pages

Global Climate Models Violate Scaling of the Observed Atmospheric Variability

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC AEROSOLS; ATMOSPHERIC TEMPERATURE; COMPUTER SIMULATION; CORRELATION METHODS; GREENHOUSE EFFECT; MATHEMATICAL MODELS;

EID: 4244112582     PISSN: 00319007     EISSN: 10797114     Source Type: Journal    
DOI: 10.1103/PhysRevLett.89.028501     Document Type: Article
Times cited : (116)

References (21)
  • 1
    • 0034674593 scopus 로고    scopus 로고
    • H. Grassl, Science 288, 1991 (2000).
    • (2000) Science , vol.288 , pp. 1991
    • Grassl, H.1
  • 3
    • 85038326490 scopus 로고    scopus 로고
    • A typical climate module within the AOGCM machinery will have a grid spacing of 300–500 km and 10–20 vertical layers as compared to a weather forecasting model with a grid spacing of 100 km or less and 30–40 layers
    • A typical climate module within the AOGCM machinery will have a grid spacing of 300–500 km and 10–20 vertical layers as compared to a weather forecasting model with a grid spacing of 100 km or less and 30–40 layers.
  • 4
    • 85038272866 scopus 로고    scopus 로고
    • http://ipcc-ddc.cru.uea.ac.uk/dkrz/dkrz_index.html
    • http://ipcc-ddc.cru.uea.ac.uk/dkrz/dkrz_index.html.
  • 6
    • 85038305642 scopus 로고    scopus 로고
    • The models also predict climate warming with a global mean increase during the 21st century, in the range of (Formula presented) for greenhouse gas forcing only and (Formula presented) for greenhouse gas plus sulphate aerosol forcing, depending upon the model
    • The models also predict climate warming with a global mean increase during the 21st century, in the range of (Formula presented) for greenhouse gas forcing only and (Formula presented) for greenhouse gas plus sulphate aerosol forcing, depending upon the model.
  • 10
    • 34547856203 scopus 로고
    • C.-K. Peng, Phys. Rev. E 49, 1685 (1994).
    • (1994) Phys. Rev. E , vol.49 , pp. 1685
  • 19
    • 0004240525 scopus 로고
    • Springer, New York
    • Fractals in Science, A. Bunde and S. Havlin (Springer, New York, 1995).
    • (1995) Fractals in Science
  • 20
    • 0038261541 scopus 로고
    • Plenum Press, New York
    • J. Feder, Fractals (Plenum Press, New York, 1989).
    • (1989) Fractals
    • Feder, J.1
  • 21
    • 85038340533 scopus 로고    scopus 로고
    • The large differences between FA and DFA reemphasize that FA (as the Hurst method) cannot be used by itself for evaluating the scaling exponent
    • The large differences between FA and DFA reemphasize that FA (as the Hurst method) cannot be used by itself for evaluating the scaling exponent.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.