<DIF xmlns="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/ http://gcmd.gsfc.nasa.gov/Aboutus/xml/dif/dif_v9.8.4.xsd">
  <Entry_ID>noaa-lakelevel-23074</Entry_ID>
  <Entry_Title>New Long Pond, Massachesetts Lake Level data during the Holocene</Entry_Title>
  <Data_Set_Citation>
    <Dataset_Creator>Newby, P.E.; Donnelly, J.P.; Shuman, B.N.; MacDonald, D.</Dataset_Creator>
    <Dataset_Title>New Long Pond, Massachesetts Lake Level data during the Holocene</Dataset_Title>
    <Dataset_Release_Date>2017-11-15</Dataset_Release_Date>
    <Dataset_Publisher>NCDC-Paleoclimatology</Dataset_Publisher>
    <Data_Presentation_Form>ONLINE Files</Data_Presentation_Form>
    <Dataset_DOI>Pending</Dataset_DOI>
    <Online_Resource>https://www.ncdc.noaa.gov/paleo/study/23074</Online_Resource>
  </Data_Set_Citation>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>P.E.</First_Name>
    <Last_Name>Newby</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>J.P.</First_Name>
    <Last_Name>Donnelly</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>B.N.</First_Name>
    <Last_Name>Shuman</Last_Name>
  </Personnel>
  <Personnel>
    <Role>Investigator</Role>
    <First_Name>D.</First_Name>
    <Last_Name>MacDonald</Last_Name>
  </Personnel>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>age,null,null,calendar year before present,null,climate reconstructions|lake levels|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,range upper bound,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,null,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,Elevation below modern; Multi-core sediment stratigraphy constrains lake elevation</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,range lower bound,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,Elevation below modern; Multi-core sediment stratigraphy constrains lake elevation</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,range upper bound,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,Elevation below modern; Multi-core sediment stratigraphy constrains lake elevation</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,range lower bound,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>lake level,null,null,centimeter,null,climate reconstructions|lake levels|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>climate reconstructions|lake levels|paleolimnology</Term>
    <Detailed_Variable>age,null,null,year Common Era,null,climate reconstructions|lake levels|paleolimnology,null,null,N,null</Detailed_Variable>
  </Parameters>
  <Parameters>
    <Category>earth science</Category>
    <Topic>paleoclimate</Topic>
    <Term>lake levels</Term>
  </Parameters>
  <ISO_Topic_Category>geoscientificInformation</ISO_Topic_Category>
  <Keyword>Other Hydroclimate Reconstruction</Keyword>
  <Paleo_Temporal_Coverage>
    <Paleo_Start_Date>11900 cal yr BP</Paleo_Start_Date>
    <Paleo_Stop_Date>50 cal yr BP</Paleo_Stop_Date>
  </Paleo_Temporal_Coverage>
  <Data_Set_Progress>Complete</Data_Set_Progress>
  <Spatial_Coverage>
    <Southernmost_Latitude>41.85</Southernmost_Latitude>
    <Northernmost_Latitude>41.85</Northernmost_Latitude>
    <Westernmost_Longitude>-70.6777</Westernmost_Longitude>
    <Easternmost_Longitude>-70.6777</Easternmost_Longitude>
    <Minimum_Altitude>29</Minimum_Altitude>
    <Maximum_Altitude>29</Maximum_Altitude>
  </Spatial_Coverage>
  <Location>
    <Location_Category>Continent</Location_Category>
    <Location_Type>North America</Location_Type>
    <Location_Subregion1>United States Of America</Location_Subregion1>
    <Location_Subregion2>Massachusetts</Location_Subregion2>
    <Detailed_Location>New Long Pond, Massachusetts&gt;LATITUDE 41.85&gt;LONGITUDE -70.6777</Detailed_Location>
  </Location>
  <Access_Constraints>None</Access_Constraints>
  <Use_Constraints>Please cite original publication, online resource, dataset and publication DOIs (where available), and date accessed when using downloaded data. If there is no publication information, please cite investigator, title, online resource, and date accessed. The appearance of external links associated with a dataset does not constitute endorsement by the Department of Commerce/National Oceanic and Atmospheric Administration of external Web sites or the information, products or services contained therein. For other than authorized activities, the Department of Commerce/NOAA does not exercise any editorial control over the information you may find at these locations. These links are provided consistent with the stated purpose of this Department of Commerce/NOAA Web site.</Use_Constraints>
  <Data_Set_Language>English</Data_Set_Language>
  <Data_Center>
    <Data_Center_Name>
      <Short_Name>DOC/NOAA/NESDIS/NCEI</Short_Name>
      <Long_Name>National Centers for Environmental Information, NESDIS, NOAA, U.S. Department of Commerce </Long_Name>
    </Data_Center_Name>
    <Data_Center_URL>https://www.ncdc.noaa.gov/data-access/paleoclimatology-data</Data_Center_URL>
    <Personnel>
      <Role>DATA Center Contact</Role>
      <First_Name>Bruce</First_Name>
      <Last_Name>Bauer</Last_Name>
      <Email>bruce.a.bauer@noaa.gov</Email>
      <Email>paleo@noaa.gov</Email>
      <Phone>303-497-6280</Phone>
      <Fax>303-497-6513</Fax>
      <Contact_Address>
        <Address>325 Broadway, E/NE31</Address>
        <City>Boulder</City>
        <Province_or_State>CO</Province_or_State>
        <Postal_Code>80305-3328</Postal_Code>
        <Country>USA</Country>
      </Contact_Address>
    </Personnel>
  </Data_Center>
  <Distribution>
    <Distribution_Media>online</Distribution_Media>
    <Distribution_Format>ASCII</Distribution_Format>
  </Distribution>
  <Reference>
    <Author>Newby, Paige E., Jeffrey P. Donnelly, Bryan N. Shuman, and Dana MacDonald</Author>
    <Publication_Date>2009</Publication_Date>
    <Title>Evidence of centennial-scale drought from southeastern Massachusetts during the Pleistocene/Holocene transition</Title>
    <Series>Quaternary Science Reviews</Series>
    <Volume>28</Volume>
    <Issue>17-18</Issue>
    <Pages>1675-1692</Pages>
    <DOI>10.1016/j.quascirev.2009.02.020</DOI>
  </Reference>
  <Reference>
    <Author>Newby, Paige E., Bryan N. Shuman, Jeffrey P. Donnelly, Kristopher B. Karnauskas, and Jeremiah Marsicek</Author>
    <Publication_Date>2014</Publication_Date>
    <Title>Centennial-to-millennial hydrologic trends and variability along the North Atlantic Coast, USA, during the Holocene</Title>
    <Series>Geophysical Research Letters</Series>
    <Volume>41</Volume>
    <Issue>12</Issue>
    <DOI>10.1002/2014GL060183</DOI>
  </Reference>
  <Summary>
    <Abstract>A principal method for studying past hydroclimatic change is the reconstruction of paleo-lake levels. Here, we provide high-resolution lake-level records from New Long Pond and Rocky Pond in southeastern Massachusetts, which each contain evidence for multiple, sub-centennial-to-millennial scale low stands during the transition between the Late Pleistocene (15.0 ka) and Middle Holocene (ca 7.0 ka). Data from New Long Pond also demonstrate sedimentary evidence for a drop in water levels in the early to mid AD 20th century, when long-term trends in instrumental data show lower-than-average precipitation in the northeastern United States. Local data show the most precipitous declines in precipitation and groundwater levels are concurrent with the most severe drought in the AD 1960s, which occurred during a period of low sea-surface temperatures in the western North Atlantic. Ground penetrating radar and sediment core data indicate five intervals with numerous paleo-shoreline deposits between ca 15.0 and 7.0 ka, similar to the layer deposited in the AD 1960s. Many of the intervals of low lake levels coincide with proposed meltwater release events or abrupt climate oscillations in the circum North Atlantic. For example, we document at least three low stands during the Younger Dryas (12.9-11.6 ka) and in association with the &quot;9.2&quot; and &quot;8.2&quot; ka events. The combined evidence of (1) concurrent paleo-droughts in southeastern New England with documented North Atlantic abrupt cooling events and (2) recent drought with the modern association of low sea-surface temperatures indicates that freshening and cooling of the western North Atlantic is a viable mechanism for decreasing moisture within the region. Large-scale changes in seasonality and ice sheet extent also may have increased the susceptibility of the northeast to dry conditions triggered by changes in the North Atlantic. 
          STUDY NOTES: Lake level units are in &quot;cm below modern level&quot;, so positive values indicate a drop in lake level. Contributed as part of the PAGES2k North American Hydroclimate synthesis project.</Abstract>
  </Summary>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/pages2k/NAm2kHydro-2017/data-version-1.0.0/NewLong.Newby.2014.lpd</URL>
    <Description>Linked Paleo Data (LiPD) File Format; New Long Pond Lake Level Data</Description>
  </Related_URL>
  <Related_URL>
    <URL_Content_Type>
      <Type>GET DATA</Type>
    </URL_Content_Type>
    <URL>https://www1.ncdc.noaa.gov/pub/data/paleo/pages2k/NAm2kHydro-2017/noaa-templates/data-version-1.0.0/NewLong.Newby.2014.txt</URL>
    <Description>NOAA Template File; New Long Pond Lake Level Data</Description>
  </Related_URL>
  <IDN_Node>
    <Short_Name>USA/NOAA</Short_Name>
  </IDN_Node>
  <Metadata_Name>DIF</Metadata_Name>
  <Metadata_Version>Version 9.8.4</Metadata_Version>
  <DIF_Creation_Date>2018-12-11</DIF_Creation_Date>
  <Last_DIF_Revision_Date>2018-12-11</Last_DIF_Revision_Date>
</DIF>
