Simmonds, 2009: Cold events over Southern Australia: Synoptic climatology and hemispheric structure.
Mcintosh, 2011: The synoptic climatology of cool-season rainfall in the central wheatbelt of Western Australia.
The main principle of synoptic climatology methods applied in the present study is that the variety of atmospheric circulation can be classified into a relatively small number of CTs (Barry & Perry, 1973; Yarnal, 1993; Huth et al.
An important feature of synoptic climatology is a smaller spatial range compared to NAO and other similar indices that describe atmospheric circulation over continents.
The basic paradigm of synoptic climatology that the atmospheric circulation determines local meteorological conditions has been proved by numerous studies (Barry & Perry, 1973; Yarnal, 1993; Barry & Carleton, 2001).
Figure 1, which shows the November synoptic climatology, also illustrates two opposing processes that affect winter roads.
Heavy cold-season precipitation in the Northwestern United States: Synoptic climatology and an analysis of the flood of 17-18 January 1986.
A synoptic climatology of surface-level ozone in Eastern Wisconsin, USA.
Developments and prospects in synoptic climatology.
The purpose of this study is to use synoptic climatology to understand the processes which produce this diurnal rainfall pattern.
A synoptic climatology for environmental baseline analysis.
Gyakum, 1999: Heavy cold-season precipitation in the northwestern United States: Synoptic climatology
and an analysis of the flood of 17-18 January 1986.