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<H2 align=3Dcenter>SUPPLEMENTAL INFORMATION...IN GREATER DEPTH</H2>
<H4 align=3Dcenter>To complement the Daily Summary for Friday, 2 October =
2009=20
</H4>
<H4 align=3Dcenter>INDIAN SUMMER, FIRST FROST AND GROWING SEASON</H4>
<HR>

<P>As we approach the first week of October, many residents in the =
northern half=20
of the country will become keenly aware of the approach of winter, with =
the=20
rapid shrinking of the daylight duration and the rapid decrease in the =
daily=20
average temperatures. With the first frost, autumn marks the end of the =
growing=20
season for many of the crops and plants through many areas of the =
country. Many=20
of us may also experience "Indian Summer". </P>
<H4>INDIAN SUMMER</H4>
<P>During early to mid autumn, a frequently occurring spell of warm =
weather may=20
occur across the Northeast quadrant of the country. This sequence of =
days marked=20
by pleasant weather is often called "Indian Summer" in North America. =
While the=20
origin of the term is somewhat uncertain, one of the accepted legends =
dating=20
back to late 18th century New England suggests that Native Americans =
used this=20
warm spell in autumn for harvesting and preparing their lodges for the=20
forthcoming winter. </P>
<P>This weather event is marked by warm, hazy and sunny days, with cool =
nights=20
that usually follow the first autumn frost. In fact, purists maintain =
that a=20
true Indian Summer can only occur following the first killing frost in =
autumn.=20
While this argument may be true at least in New England and the =
Northeast, other=20
areas of the country can claim a similar type of quiet and warm weather =
spell,=20
but without the need for a freeze. </P>
<P>Usually, American Indian Summer occurs in October and may extend into =

November, following several cold outbreaks during late September. At =
this time,=20
the atmospheric circulation regime is undergoing a change from a late =
summer=20
pattern to more of an early winter one. The cold outbreaks during late =
September=20
occur as the source for cold Canadian air masses become established and =
storm=20
activity increases. The cold air behind the cold fronts that invade the =
Great=20
Lakes and Northeast often provide the needed killing frost. Frequently =
during=20
October, large high-pressure systems move slowly across the country. A =
large=20
high-pressure system that remains anchored over the southeastern U.S. =
sets the=20
stage for Indian Summer in the Midwest and Northeast. Light winds from =
the=20
desert Southwest on the west and north flanks of the high-pressure =
system keep=20
conditions mild over the Mississippi Valley, Great Lakes and into the =
Northeast,=20
including New England. Since the flow of air is not directly from the =
Gulf of=20
Mexico, the air is not hot and muggy. The high-pressure system is =
relatively=20
stable, in that both mixing and cloud formation are suppressed, leading =
to hazy,=20
but relatively cloud-free days. Nighttime temperatures cool readily =
because of=20
the low moisture content in the air and weak winds as well as the longer =

duration of darkness. </P>
<H4>AN END TO THE GROWING SEASON</H4>
<P>Many crops are sensitive to the weather, in particular to extremes in =
air=20
temperature. Frost sensitive plants, such as tomatoes, peppers, and =
cucumbers,=20
freeze when the temperature falls to 28 degrees Fahrenheit, while apples =
are=20
damaged when the temperature drops below 20 degrees. A killing freeze =
occurs=20
when widespread damage to crops terminates the growing season. </P>
<P>In most mid latitude climates, the growing season is often used =
synonymously=20
with the frost-free season, loosely defined as the length of time =
between the=20
last killing frost in spring and the first killing frost in the autumn. =
While=20
the exact time span would vary by plant type, the growing season is =
often=20
related to the interval when the daily minimum temperature remains above =
32=20
degrees. </P>
<P>The National Weather Service issues several non-precipitation weather =

advisories and warnings to inform the public of the potential for damage =
to=20
agricultural crops and other vegetation as a consequence of cold =
weather. These=20
advisories and warnings are only issued during the growing season when =
the=20
greatest threat to agriculture would occur. </P>
<UL>
  <LI>A <B>freeze warning</B> is issued during the growing season to =
warn the=20
  public when the near surface temperatures are anticipated to fall well =
below=20
  freezing over a wide spread area for a significant length of time. =
These=20
  warnings are issued regardless of whether frost is expected to form.=20
  <LI>A<B> frost advisory</B> is issued during the growing season to =
alert the=20
  public that wide spread frost is expected . Typically, overnight low=20
  temperatures in the 30s can result in the occurrence of widespread =
frost,=20
  especially in conjunction with light winds and clear skies. </LI></UL>
<HR>

<P><I>Return to the <A=20
href=3D"http://www.ametsoc.org/amsedu/online/archive/course/09_fall/f09w0=
4f_sum.html">Friday=20
Daily Weather Summary </A></I></P>
<ADDRESS>Prepared by Edward J. Hopkins, Ph.D., email <A=20
href=3D"mailto:hopkins@meteor.wisc.edu">hopkins@meteor.wisc.edu</A> =
<BR>=A9=20
Copyright, 2009, The American Meteorological Society. =
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