Statistics in the environmental and earth sciences edited by A.T. Walden and P. Guttorp Edward Arnold, 1992, £49.50
Global Environmental Change Elsevier 4:2 (1994) 174-175
Investigating the origins and significance of low‐frequency modes of climate variability
Geophysical Research Letters 21:10 (1994) 883-886
Abstract:
An analysis of the 130‐year record of the Earth's global mean temperature reveals a significant warming trend and a residual consistent with an auto‐correlated (“red”) noise process whose predictability decays with a timescale of two years. Thus global temperatures, in isolation, do not indicate oscillations at 95% confidence against a red noise null hypothesis. Weak signals identified in the global series can, however, be traced to significant sea surface temperature oscillations in the equatorial Atlantic (period ∼10 years) and the El Niño region of the Pacific (3–5 years). No robust evidence is found in this data for interdecadal oscillations, The 10‐year Atlantic oscillation corresponds to a pattern of temperature anomalies which has been associated with interannual variations in West African rainfall and in U.S. hurricane landfall frequency. Copyright 1994 by the American Geophysical Union.CLIMATE SENSITIVITY AND TROPICAL MOISTURE DISTRIBUTION
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 99:D2 (1994) 3707-3716
SST measurements from ATSR on ESA's ERS-1 satellite-early results
Institute of Electrical and Electronics Engineers (IEEE) (1993) 155-156 vol.1