<?xml version="1.0" encoding="UTF-8"?>
<resource xmlns="http://datacite.org/schema/kernel-4" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.1/metadata.xsd">
  <identifier identifierType="DOI">10.18453/rosdok_id00001352</identifier>
  <creators>
    <creator>
      <creatorName nameType="Personal">Kaifler, Bernd</creatorName>
      <givenName>Bernd</givenName>
      <familyName>Kaifler</familyName>
      <nameIdentifier nameIdentifierScheme="GND" schemeURI="http://d-nb.info/gnd/">http://d-nb.info/gnd/142386383</nameIdentifier>
    </creator>
  </creators>
  <titles>
    <title>Thermal structure and gravity waves in the Antarctic middle atmosphere observed by lidar</title>
    <title>Lidar-Messungen der thermischen Struktur und Untersuchung von Schwerewellen in der antarktischen mittleren Atmosphäre</title>
  </titles>
  <publisher>Universität Rostock</publisher>
  <publicationYear>2014</publicationYear>
  <resourceType resourceTypeGeneral="Text" />
  <subjects>
    <subject xml:lang="en" schemeURI="http://dewey.info/" subjectScheme="dewey">530 Physics</subject>
  </subjects>
  <dates>
    <date dateType="Created">2014</date>
  </dates>
  <language>en</language>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="PURL">http://purl.uni-rostock.de/rosdok/id00001352</alternateIdentifier>
    <alternateIdentifier alternateIdentifierType="URN">urn:nbn:de:gbv:28-diss2014-0104-4</alternateIdentifier>
  </alternateIdentifiers>
  <descriptions>
    <description descriptionType="Abstract">The IAP iron Doppler lidar has been operated at the Antarctic station Davis (69°S, 78°E) between December 2010 and December 2012. Seasonal variations in the thermal structure above Davis are studied and wave-induced temperature perturbations are analyzed on different time scales. Gravity wave potential energy densities (GWPED) are computed from stratospheric and mesospheric lidar observations and compared to a simple gravity wave model. It is shown that observed seasonal variations in GWPED are caused by selective filtering of zonally propagating gravity waves.</description>
  </descriptions>
</resource>
