Some of
the largest snow totals were: 36.0 inches (91.4 cm) in Hudson, Massachusetts; 33.5 inches (85.1 cm) in Thompson, Connecticut; 33.2 inches (84.3 cm) in Nashua, New Hampshire; 31.5 inches (80.0 cm) in Sanford, Maine; 30.0 inches (76.2 cm) in Orient, New York; and 28.5 inches (72.4 cm) in Burrillville, Rhode Island.
Not exact matches
With
total privacy and stunning views of Penobscot Bay and the islands of the Mid-Coast, as well as the Camden Hills, Hosmer Pond, and the Camden
Snow Bowl, every one of the many
large windows looks out onto something picturesque in all directions.
Wili: As ice volume decreases, the fraction of volume which is new ice increases, and hence the year to year variability in new ice becomes a
larger fraction of the
total ice volume variability, so I don't think the smoothed downward slope will stay as smooth, i.e. you should expect bigger surprises to the upside on a given winter if it is cold and has heavy
snow fall.
For the entire Northern Hemisphere, there is evidence of an increase in both storm frequency and intensity during the cold season since 1950,1 with storm tracks having shifted slightly towards the poles.2, 3 Extremely heavy snowstorms increased in number during the last century in northern and eastern parts of the United States, but have been less frequent since 2000.11,15
Total seasonal snowfall has generally decreased in southern and some western areas, 16 increased in the northern Great Plains and Great Lakes region, 16,17 and not changed in other areas, such as the Sierra Nevada, although
snow is melting earlier in the year and more precipitation is falling as rain versus
snow.18 Very snowy winters have generally been decreasing in frequency in most regions over the last 10 to 20 years, although the Northeast has been seeing a normal number of such winters.19 Heavier - than - normal snowfalls recently observed in the Midwest and Northeast U.S. in some years, with little
snow in other years, are consistent with indications of increased blocking (a
large scale pressure pattern with little or no movement) of the wintertime circulation of the Northern Hemisphere.5 However, conclusions about trends in blocking have been found to depend on the method of analysis, 6 so the assessment and attribution of trends in blocking remains an active research area.
CL at # 45 wrote: «As ice volume decreases, the fraction of volume which is new ice increases, and hence the year to year variability in new ice becomes a
larger fraction of the
total ice volume variability, so I don't think the smoothed downward slope will stay as smooth, i.e. you should expect bigger surprises to the upside on a given winter if it is cold and has heavy
snow fall.»
The effect continues, but the
larger total area of the snowball means even more
snow is accumulated.