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Volumn 68, Issue 4 2, 2003, Pages 461331-461335

Power-law persistence and trends in the atmosphere: A detailed study of long temperature records

Author keywords

[No Author keywords available]

Indexed keywords

APPROXIMATION THEORY; ATMOSPHERIC TEMPERATURE; CORRELATION METHODS; EARTH ATMOSPHERE; GLOBAL WARMING; POLYNOMIALS; PROBABILITY DISTRIBUTIONS; RANDOM PROCESSES; WAVELET TRANSFORMS; WEATHER FORECASTING;

EID: 0348195678     PISSN: 1063651X     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article
Times cited : (209)

References (29)
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    • Pelletier, J.D.1    Turcotte, D.L.2
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    • P. Talkner and R.O. Weber, Phys. Rev. E 62, 150 (2000); J. Geophys. Res., [Atmos.] 106, 20131 (2001).
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    • Talkner, P.1    Weber, R.O.2
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    • Plenum, New York
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    • S. Lovejoy and D. Schertzer, Nonlinear Variability in Geophysics: Scaling and Fractals (Kluwer Academic Publishers, Dordrecht, MA, 1991); D. Lavallee, S. Lovejoy, and D. Schertzer, in Fractals in Geography, edited by L. DeCola and N. Lam (Prentice-Hall, Englewood Cliffs, NJ, 1993), pp. 158-192; G. Pandey, S. Lovejoy, and D. Schertzer, J. Hydrol. 208, 62 (1998).
    • (1991) Nonlinear Variability in Geophysics: Scaling and Fractals
    • Lovejoy, S.1    Schertzer, D.2
  • 25
    • 0027801793 scopus 로고
    • edited by L. DeCola and N. Lam (Prentice-Hall, Englewood Cliffs, NJ)
    • S. Lovejoy and D. Schertzer, Nonlinear Variability in Geophysics: Scaling and Fractals (Kluwer Academic Publishers, Dordrecht, MA, 1991); D. Lavallee, S. Lovejoy, and D. Schertzer, in Fractals in Geography, edited by L. DeCola and N. Lam (Prentice-Hall, Englewood Cliffs, NJ, 1993), pp. 158-192; G. Pandey, S. Lovejoy, and D. Schertzer, J. Hydrol. 208, 62 (1998).
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    • S. Lovejoy and D. Schertzer, Nonlinear Variability in Geophysics: Scaling and Fractals (Kluwer Academic Publishers, Dordrecht, MA, 1991); D. Lavallee, S. Lovejoy, and D. Schertzer, in Fractals in Geography, edited by L. DeCola and N. Lam (Prentice-Hall, Englewood Cliffs, NJ, 1993), pp. 158-192; G. Pandey, S. Lovejoy, and D. Schertzer, J. Hydrol. 208, 62 (1998).
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    • note
    • The crossover increases, as an artefact of the DFA method, with increasing order of DFA. DFA0 and DFA1 give the best estimate for the crossover (see also Refs. [9-11]).


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.