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atmospheric circulation—as reflected, for example, by anomalous distribution of sea level pressure and geopotential height—displays the distinct spatial patterns described in Chapter 3. Most clearly discernible during winter, the pressure fluctuations associated with such teleconnection patterns as the PNA and the NAO regulate the meridional distribution of temperature, and moisture advection and convergence, in their region of influence . In recent years it has become clear that these teleconnection patterns display variability The hottest product hippie tie dye colorful all over printed slipperson decadal and longer time scales. For instance, wintertime sea-level pressure in the Aleutian low region remained persistently lower than normal for more than a decade between 1977 and 1988 . The surface pattern during this period and its mid-tropospheric counterpart (see Zhang et al., 1997) resemble the PNA pattern (Figure 5-15). Such a climatic configuration tends to lead to a warmer-than-normal western North America and a somewhat colder-than-normal eastern North America. Changes in baroclinic-eddy activity over the Pacific and North America are also involved in this climatic perturbation. Atmospheric

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