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The growing season is considered by some to be a simple and yet significant indicator of the impact of hemispheric temperature variations at the local level. Yet, the effect of the use of different definitions of the growing season has never been determined.In the present paper, time series of the length of differently defined growing seasons at four Wisconsin stations are compared. The results show that their lengths have fluctuated in a variety of patterns over the past 80 years. Two growing seasons which showed a significant trend did not agree on its direction. The reason for this disparity is that trends in maximum and minimum temperatures are not necessarily of the same sign at different times of the year. These findings suggest that the length of the growing season is not the simple climatic indicator it has been assumed to be.

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The association between daily as well as monthly winter precipitation and concurrent 700 hPa heights for 3 different North American precipitation regimes was examined using correlation fields and a typing of daily 700 hPa height patterns. Wet days, regardless of circulation type, were found to be associated with negative height anomalies immediately to the west or northwest of the precipitation regions, at the 'local' grid point. These small-scale height anomalies were found to represent traveling short waves that were missed by the circulation typing scheme. The correlation fields between monthly precipitation and concurrent 700 hPa heights revealed a westward shift of the height minima to a location west of 100°W, to a 'remote' grid point. The nature of these remote minima was examined using the 10 wettest and 10 driest months. Decomposition of the height anomalies at the remote grid points into between-type and within-type contributions revealed that while some of the negative heights during wet months are due to an increase in the frequency of circulation patterns with below normal heights (such as troughs or weak ridges), more than two-thirds of the contribution comes from height depressions superimposed upon the larger-scale patterns and most of these are associated with positive vorticity. This leads to the conclusion that the correlation minima west of 100°W at the monthly time scale reflect the frequent generation of short waves during wet months over the well-known North American cyclogenetic region east of the Rocky Mountains. These results have 2 implications with respect to statistical downscaling. First, regarding techniques designed to extract information from a single grid point: the optimum grid point location may be a function of the time scale under consideration. Second, regarding techniques designed to extract information from large-scale circulation patterns: the difficulties in capturing the very important but small short waves limit their usefulness. KEY WORDS: Precipitation · 700 hPa · Circulation pattern typing · North America · DownscalingResale or republication not permitted without written consent of the publisher Clim Res 21: 27-42, 2002 cal to this approach since the circulation features of significance to the local climate need to be captured. Most investigators place the window over and to the west of the area of interest because weather systems travel from west to east. Using information from the nearest grid point also makes physical sense because the atmospheric conditions at the nearest point should be most similar to those over the area of interest. However, it has been shown that for some parts of the country the strongest correlation between local precipitation and geopotential heights is not at the nearest (local) but at a remote grid point (generally to the west of the area of interest).Specifically, Stidd (1954) computed correlation fields between 700 hPa heights and a series of state-wide precipitation totals for winter months and found that almost all of ...