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V       "Card, Robert" <Robert.Card §hq.dae.gav>
       A           06/0212003 07:49:18 AM

Record Type:    RecordMhoy

To:      Phil Cooney/CEQ/EOP~EOP, "James Mhey(E-mail)" <James.R.Mahoney~noaa.gov>
cc:
Subject: FW: 20th Century Climate Not So Hot



I assume you all saw this but just in case.

…---OriginalMessage ---
From: Richard Seibert [mnailto:rseibert~annctr.org
Sent: Friday, May 30, 2003 10:59 AM
Subject: 20th Century Climate Not So Hot



Harvard ShieldSmithsonian Sunburst
Harvard-Smithsonian Center for Astrophysics
Press Release


[red bar] <http:I/cfa-www.harvardl.edul> [CfA Hor e]
<http://cfa-www.harvard.edu/flewtop/search.html> [CfA Search]
<http://cfa-www.harvard.edu/lev~top/cfahelp.htmI- [CfA Help]

Release No.: 03-10
For Release: March 31, 2003

20th Century Climate Not So Hot

Cambridge, MA - A review of more than 200 clime te studies led by researchers
at the Harvard-Smithsonian Center for Astrophysi s has determined that the
20th century is neither the warmest century nor th E)century with the most
extreme weather of the past 1000 years. The revipw also confirmed that the
Medieval Warm Period of 800 to 1300 A.D. and tl e Little Ice Age of 1300 to
1900 A.D. were worldwide phenomena not limnite to the European and North
American continents. While 20th century tempera res are much higher than in
the Little Ice Age period, many parts of the world show the medieval warmth
to be greater than that of the 20th century.
Smithsonian astronomers Willie Soon and Sallie Baliunas, with co-authors
Craig ldso and Sherwood ldso (Center for the StLudy of Carbon Dioxide and
Global Change) and David Legates (Center for Climatic Research, University
of Delaware), compiled and examined results from more than 240 research
papers published by thousands of researchers o er the past four decades.
Their report, covering a multitude of geophysical ~nd biological climate
indicators, provides a detailed look at climate chahges that occurred in
 different regions around the world over the last   idoij years.
 "Many true research advances in reconstructing ncient climates have
time to
occurred over the past two decades," Soon says, "s we felt it was
pull together a large sample of      recent studies from :he last 5-1 0 years and
look for patterns of variability and change. In fact, clear patterns
                                                                         did
emerge showing that regions        worldwide experienced the highs of the Medieval
Warm Period and lows of the Little Ice Age, and that 20th century
temperatures are generally cooler than during the rjiedieval warmth."          the
Soon and his colleagues concluded that the 2Oth c ntury is neither Their
warmest century over the last 1000        years, nor is it 5he most extreme.
                                                                           make
findings about the pattern of historical climate vani ~tions will help
 computer climate models simulate         both natural andI man-made changes more
                                                                              and
 accurately, and lead to better climate forecasts esoiecially on local
 regional levels. This is especially true in simulationh on timescales
 ranging from several decades to a century.
 Historical Cold, Warm Periods Verified
                                                                            not the
 Studying climate change is challenging for a number of reasons,
  least of which is the bewildering    variety of climate idicators - all
  sensitive to different climatic variables, and each cperating on slightly
                                                                          tree ring
  overlapping yet distinct scales of space and time. l~r example,
                                                                           trends,
  studies can yield yearly records of temperature an precipitation
  while glacier ice cores record those variables over       longer time scales of
  several decades to a century.I
  Soon, Baliunas and colleagues analyzed numerou climate indicators
   including: borehole data; cultural data; glacier advhnces or retreats; tree or
   geomorphology; isotopic analysis from lake sediments or ice cores,     fossils;
   peat celluloses (carbohydrates), corals, stalagmit4 or biological
   net ice accumulation    rate, including dust or chemical counts; lake fossils
   and sediments; river sediments; melt layers in ice cores; phenological
   (recurring natural phenomena in relation to climate) and paleontological     growth,
   fossils; pollen; seafloor sediments; luminescent analysis; tree ring
   including either ring width or maximum      late-wood density; and shifting tree
   line positions plus tree stumps in lakes, marshes and streams.
                                                                            order to
   "Like forensic detectives, we assembled these se 1es of clues in                Is there
    answer a specific question about local and region I climate change: over
    evidence for notable climatic anomalies during pqrticular      time periods
                                                                                    that such
    the past 1000 years?" Soon says. "The cumulative evidence showed
    anomalies did exist.''"
                                                                               climate
    The worldwide range of climate records confirmeli two significant
    periods in the last thousand    years, the Little Ice a~g the Medieval Warm
                                                               and
                                                                             tol1900
     Period. The climatic notion of a Little Ice Age intehal from 1300
     A.D. and a Medieval   Warm Period from 800 to 13aoo A.D. appears to be rather
                                                                             one region to
     well-confirmed and wide-spread, despite some differences from
                                                                                 drought
     another as measured by other climatic variables ike precipitation,
     cycles, or glacier advances and retreats.
                                                                                  supporting
     "For a long time, researchers have possessed a ecdotal evidence
     the existence of these climate    extremes," Baliun s says. "For example, the
                                                                                second
     Vikings established colonies in Greenland at the beginning of the
      millennium that died  out several hundred years I tar when the climate turned
                                                                                     warmth.
      colder. And in England, vineyards had flourished during the medieval
      Now, we have an accumulation of objective data        to back up these cultural
      indicators."
                                                                                  in the
      The different indicators provided clear evidence 'or a warm period
      Middle Ages. Tree ring summer      temperatures sl owed a warm interval from 950
                                                                                          to
      A.D. to I1100 A.D. in the northern high latitude zc nes, which corresponds
                                                                           from 14
      the "Medieval Warm Period." Another database ) tree growth
                                                                            similar early
      different locations over 30-70 degrees north latituide showed a to be greater
      warm period. Many parts of the world show the A       medievai warmth
eerh      h
              -
than that of the 20th century.
                                                aSinii
                                                     cetfc eerh h
The study funded by NASA, the Air Force Officeor hnd the American Petroleum
         -
National Oceanic and Atmospheric Administration,           journal. A seo
Institute will be published in the Energy and Envirjnment 31, 2003 isseo
shorter  paper by Soon and Baliunas   appeared in tile January
the Climate Research journal.I
                                                indicators are available online at
NOTE TO EDITORS: Photos of key climate                  Il
http://cfa-www~harvard.edu/press/prSl 3 Oimage.ht
<http://cfa-www.harvard.edu/press/prO I oimnage.hjml>
                                                   the IHarvard-Smithsonian Center
 Headquartered in Cambridge, Massachusetts,
                                                 between the Smithsonian
 for Astrophysics (CTA) is a joint collaborationColleg E Observatory. CfA
 Astrophysical Observatory and the Harvard
                                                    study the origin,
 scientists organized into six research divisions
 evolution, and ultimate fate  of the universe.
 For more information, contact:
 David Aguilar, DirectorCenter for Affairs
                         of Public
                                   Astrophysics
 Harvard-Smithsonian Fax: 617-495-7468
 Phone: 617-495-7462         <mailto:daguilar~cfa. arvard.edu>
 daguilar~cfa.harvard.edu
 Christine Lafon
 Public Affairs Specialist
  Harvard-Smithsonian Center for Astrophysics
  Phone: 617-495-7463, Fax: 617-495-7016
  clafon~cfa.harvard.edu <mailto:clafon@Cfa.harvard.edu>
                                                     EST
  Last modified on Monday, 31-Mar-2003 15:18:29 a.harvard.edui
  Comments or Questions? Contact       pubaffairs~cf
  <mailto:pubaffairs@Cfa.harvard ,edu>




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RCEC Email 6.2.03

  • 1. V "Card, Robert" <Robert.Card §hq.dae.gav> A 06/0212003 07:49:18 AM Record Type: RecordMhoy To: Phil Cooney/CEQ/EOP~EOP, "James Mhey(E-mail)" <James.R.Mahoney~noaa.gov> cc: Subject: FW: 20th Century Climate Not So Hot I assume you all saw this but just in case. …---OriginalMessage --- From: Richard Seibert [mnailto:rseibert~annctr.org Sent: Friday, May 30, 2003 10:59 AM Subject: 20th Century Climate Not So Hot Harvard ShieldSmithsonian Sunburst Harvard-Smithsonian Center for Astrophysics Press Release [red bar] <http:I/cfa-www.harvardl.edul> [CfA Hor e] <http://cfa-www.harvard.edu/flewtop/search.html> [CfA Search] <http://cfa-www.harvard.edu/lev~top/cfahelp.htmI- [CfA Help] Release No.: 03-10 For Release: March 31, 2003 20th Century Climate Not So Hot Cambridge, MA - A review of more than 200 clime te studies led by researchers at the Harvard-Smithsonian Center for Astrophysi s has determined that the 20th century is neither the warmest century nor th E)century with the most extreme weather of the past 1000 years. The revipw also confirmed that the Medieval Warm Period of 800 to 1300 A.D. and tl e Little Ice Age of 1300 to 1900 A.D. were worldwide phenomena not limnite to the European and North American continents. While 20th century tempera res are much higher than in the Little Ice Age period, many parts of the world show the medieval warmth to be greater than that of the 20th century. Smithsonian astronomers Willie Soon and Sallie Baliunas, with co-authors Craig ldso and Sherwood ldso (Center for the StLudy of Carbon Dioxide and Global Change) and David Legates (Center for Climatic Research, University of Delaware), compiled and examined results from more than 240 research papers published by thousands of researchers o er the past four decades. Their report, covering a multitude of geophysical ~nd biological climate indicators, provides a detailed look at climate chahges that occurred in different regions around the world over the last idoij years. "Many true research advances in reconstructing ncient climates have
  • 2. time to occurred over the past two decades," Soon says, "s we felt it was pull together a large sample of recent studies from :he last 5-1 0 years and look for patterns of variability and change. In fact, clear patterns did emerge showing that regions worldwide experienced the highs of the Medieval Warm Period and lows of the Little Ice Age, and that 20th century temperatures are generally cooler than during the rjiedieval warmth." the Soon and his colleagues concluded that the 2Oth c ntury is neither Their warmest century over the last 1000 years, nor is it 5he most extreme. make findings about the pattern of historical climate vani ~tions will help computer climate models simulate both natural andI man-made changes more and accurately, and lead to better climate forecasts esoiecially on local regional levels. This is especially true in simulationh on timescales ranging from several decades to a century. Historical Cold, Warm Periods Verified not the Studying climate change is challenging for a number of reasons, least of which is the bewildering variety of climate idicators - all sensitive to different climatic variables, and each cperating on slightly tree ring overlapping yet distinct scales of space and time. l~r example, trends, studies can yield yearly records of temperature an precipitation while glacier ice cores record those variables over longer time scales of several decades to a century.I Soon, Baliunas and colleagues analyzed numerou climate indicators including: borehole data; cultural data; glacier advhnces or retreats; tree or geomorphology; isotopic analysis from lake sediments or ice cores, fossils; peat celluloses (carbohydrates), corals, stalagmit4 or biological net ice accumulation rate, including dust or chemical counts; lake fossils and sediments; river sediments; melt layers in ice cores; phenological (recurring natural phenomena in relation to climate) and paleontological growth, fossils; pollen; seafloor sediments; luminescent analysis; tree ring including either ring width or maximum late-wood density; and shifting tree line positions plus tree stumps in lakes, marshes and streams. order to "Like forensic detectives, we assembled these se 1es of clues in Is there answer a specific question about local and region I climate change: over evidence for notable climatic anomalies during pqrticular time periods that such the past 1000 years?" Soon says. "The cumulative evidence showed anomalies did exist.''" climate The worldwide range of climate records confirmeli two significant periods in the last thousand years, the Little Ice a~g the Medieval Warm and tol1900 Period. The climatic notion of a Little Ice Age intehal from 1300 A.D. and a Medieval Warm Period from 800 to 13aoo A.D. appears to be rather one region to well-confirmed and wide-spread, despite some differences from drought another as measured by other climatic variables ike precipitation, cycles, or glacier advances and retreats. supporting "For a long time, researchers have possessed a ecdotal evidence the existence of these climate extremes," Baliun s says. "For example, the second Vikings established colonies in Greenland at the beginning of the millennium that died out several hundred years I tar when the climate turned warmth. colder. And in England, vineyards had flourished during the medieval Now, we have an accumulation of objective data to back up these cultural indicators." in the The different indicators provided clear evidence 'or a warm period Middle Ages. Tree ring summer temperatures sl owed a warm interval from 950 to A.D. to I1100 A.D. in the northern high latitude zc nes, which corresponds from 14 the "Medieval Warm Period." Another database ) tree growth similar early different locations over 30-70 degrees north latituide showed a to be greater warm period. Many parts of the world show the A medievai warmth
  • 3. eerh h - than that of the 20th century. aSinii cetfc eerh h The study funded by NASA, the Air Force Officeor hnd the American Petroleum - National Oceanic and Atmospheric Administration, journal. A seo Institute will be published in the Energy and Envirjnment 31, 2003 isseo shorter paper by Soon and Baliunas appeared in tile January the Climate Research journal.I indicators are available online at NOTE TO EDITORS: Photos of key climate Il http://cfa-www~harvard.edu/press/prSl 3 Oimage.ht <http://cfa-www.harvard.edu/press/prO I oimnage.hjml> the IHarvard-Smithsonian Center Headquartered in Cambridge, Massachusetts, between the Smithsonian for Astrophysics (CTA) is a joint collaborationColleg E Observatory. CfA Astrophysical Observatory and the Harvard study the origin, scientists organized into six research divisions evolution, and ultimate fate of the universe. For more information, contact: David Aguilar, DirectorCenter for Affairs of Public Astrophysics Harvard-Smithsonian Fax: 617-495-7468 Phone: 617-495-7462 <mailto:daguilar~cfa. arvard.edu> daguilar~cfa.harvard.edu Christine Lafon Public Affairs Specialist Harvard-Smithsonian Center for Astrophysics Phone: 617-495-7463, Fax: 617-495-7016 clafon~cfa.harvard.edu <mailto:clafon@Cfa.harvard.edu> EST Last modified on Monday, 31-Mar-2003 15:18:29 a.harvard.edui Comments or Questions? Contact pubaffairs~cf <mailto:pubaffairs@Cfa.harvard ,edu> I i-mageOO.if ID -imageOO3.gif D I m gi-. I maeD-gi I mage16.g-