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dc.contributor.authorMobley, Curtis D.
dc.contributor.authorPreisendorfer, Rudolph W.
dc.date.accessioned2017-06-09T14:00:38Z
dc.date.available2017-06-09T14:00:38Z
dc.date.copyright1985/06/01
dc.date.issued1985
dc.identifier.issn0733-3021
dc.identifier.otherams-10856.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146019
dc.description.abstractThe problem of determining confidence intervals for climatic signals using data sets with spatial and temporal sampling inhomogeneities is solved by a four-step process. First, the actual data set is analysed to determine autoregressive models which are consistent with the actual data at daily, monthly and annual time scales. Second, these models are used to generate artificial, but realistic, data sets which reproduce selected statistical properties of the actual data. Third, these artificial data sets are sampled by Monte Carlo techniques to determine certain confidence interval coefficients appropriate to different fields, geographical regions, and averaging periods. Fourth, these confidence interval coefficients are used to place error bars on climatic signals derived from the actual data set. The technique is illustrated by the analysis of historical sea surface temperature and sea level pressure data in the eastern tropical Pacific Ocean.
dc.publisherAmerican Meteorological Society
dc.titleStatistical Analysis of Historical Climate Data Sets
dc.typeJournal Paper
dc.journal.volume24
dc.journal.issue6
dc.journal.titleJournal of Climate and Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1985)024<0555:SAOHCD>2.0.CO;2
dc.journal.fristpage555
dc.journal.lastpage567
dc.treeJournal of Climate and Applied Meteorology:;1985:;Volume( 024 ):;Issue: 006
dc.contenttypeFulltext


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