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Greece,
New York Climate
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| Rochester
and the Genesee valley experience a fairly humid,
continental type climate, which is strongly modified
by the proximity of the Great Lakes. Precipitation
is rather evenly distributed throughout the year
in quantity, but frequency is much higher in the
cloudy winter months than in the sunny summer
ones. Snowfall is heavy, but is highly variable
over short distances.Winters
are generally cold, cloudy and snowy across the
region...but are changeable and include frequent
thaws and rain as well. |
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Snow covers the ground more often than not from Christmas
into early March, but periods of bare ground are not
uncommon. About half of the annual snowfall comes
from the "lake effect" process and is very localized.
This feature develops when cold air crosses the warmer
lake waters and becomes saturated, creating clouds
and precipitation downwind. The exact location of
these snowbands is determined by the direction of
the wind. Areas east of Rochester receive the most
snow from this process, as northwest winds have a
longer "fetch" off lakeOntario, while areas south
of the city get somewhat less. Lake Erie can even
contribute some snow from this process if a west or
southwest wind is strong enough. Since Lake Ontario
does not freeze in most winters, this Lake Effect
machine can remain active throughout the winter.The
Rochester area is also subject to occasional general
or "synoptic" snowfalls...but the worst effects usually
pass the east. Total season snowfall ranges from 70
inches south of the city to about 90 inches in Rochester
to over 120 inches along the lake shore east of the
city. About 5O inches of this total results from general
snows, the rest is due to the lake effect machine.The
Lake does modify the extreme cold, the mercury falls
below zero on only about six nights in an average
winter, with anything below -l0 quite uncommon.
Spring
comes slowly to the region.The last frosts usually
occur by April 30 near the Lake...but as late as mid-May
south of the Thruway. The spring months are actually
our driest months statistically, due in part to the
stabilizing effect of the Lakes, although soils are
wet. Sunshine increases markedly in May.
Summers
are warm and sunny across the region. The average
temperature is in the 70 to 72 degree range. Rain
can be expected every third or fourth day, almost
always in the form of showers and thunderstorms. This
activity is more common inland than near the lake.
Completely overcast days in summer are rare. Severe
weather is not common, but a few cases of damaging
winds and small tornadoes occur each year. The greatest
risk of this type of activity is south of the Thruway.
There usually are several periods of uncomfortably
warm and muggy weather in an average summer, with
nine days reaching the 90-degree mark. Still, the
area usually experiences some of the most delightful
summer weather in the East.
Autumn
is pleasant, but rather brief. Mild and dry conditions
predominate through September and much of October,
but colder airmasses cross the Great Lakes with increasing
frequency starting in late October, and result in
a drastic increase in cloud cover across the region
in late October and early November. Although the first
frosts may not occur until late October along the
lakeshores, the first lake effect snows of the season
follow soon thereafter. ..usually by mid November.
These early snows melt off quickly, with a general
snow cover seldom established before mid-December.
The growing seassn is relatively long for the latitude,
averaging about 180 days.The long growing season,
combined with ample spring moisture and abundant summer
sunshine...is beneficial for the many fruit orchards
and wineries, especially near the Lake Ontario shore
and the Finger Lakes.
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