1960
DOI: 10.2307/520173
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A Method of Determining the Warmth and Temperateness of Climate

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Cited by 63 publications
(42 citation statements)
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“…To control for this possibility, we included a number of measures of such risk including: (i) seasonality and productivity (latitude and effective temperature), (ii) vulnerability to catastrophic storms (total cyclones, and mean and total wind speeds for those cyclones for the past 10 years), and (iii) drought risk (mean annual number of rainy days and standard deviation in daily rainfall). Effective temperature is a measure created by Bailey (1960) and used by Binford (2001) and Collard et al (2005) as a measure of ecosystem abundance (see the electronic supplementary material for details). With the exception of Hawaii, all data on cyclones were gathered from Australian Severe Weather (2009).…”
Section: Methodsmentioning
confidence: 99%
“…To control for this possibility, we included a number of measures of such risk including: (i) seasonality and productivity (latitude and effective temperature), (ii) vulnerability to catastrophic storms (total cyclones, and mean and total wind speeds for those cyclones for the past 10 years), and (iii) drought risk (mean annual number of rainy days and standard deviation in daily rainfall). Effective temperature is a measure created by Bailey (1960) and used by Binford (2001) and Collard et al (2005) as a measure of ecosystem abundance (see the electronic supplementary material for details). With the exception of Hawaii, all data on cyclones were gathered from Australian Severe Weather (2009).…”
Section: Methodsmentioning
confidence: 99%
“…Climatologists also have a long tradition of investigating regime shift phenomena [12,40,41], however, with the concern that some sudden step changes in climate time series might be artefacts of the measurement system, for example due to a change in the measurement method or a relocation of a meteorological station. Therefore, climatologists have developed so-called homogenization methods to account for measurement artefacts [20,64], and embedded this approach into general procedures for simultaneous detection of climate change and observational bias [65].…”
Section: Conclusion and Future Perspectivesmentioning
confidence: 99%
“…The present analysis of zonal climates uses the system of bioclimatology by Bailey (1960Bailey ( , 1964Bailey ( , 1966. This system has been applied intensively to modern aborescent ve ge tation in mid-latitudes (Axelrod 1965, 1968, Greller 1989, in a tropical area (Greller & Balasubramaniam 1988), and in near-shore paleontology (Hall 2002).…”
Section: E T H O D S Bioclimatic Analysis (From Greller 1989)mentioning
confidence: 99%
“…Se ve ral thermal characteristics have proved useful in distin gui shing vegetation, especially humid forests. Two of these cha racte ristics are the Warmth (W) of climate and its Tem perate ness (M), which were defined and quantified by Bailey (1960Bailey ( , 1966.…”
Section: E T H O D S Bioclimatic Analysis (From Greller 1989)mentioning
confidence: 99%