<?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_id00005166</identifier>
  <creators>
    <creator>
      <creatorName nameType="Personal">Vellalassery, Ashique</creatorName>
      <givenName>Ashique</givenName>
      <familyName>Vellalassery</familyName>
      <nameIdentifier nameIdentifierScheme="GND" schemeURI="http://d-nb.info/gnd/">http://d-nb.info/gnd/1392749670</nameIdentifier>
      <nameIdentifier nameIdentifierScheme="ORCID" schemeURI="https://orcid.org/">https://orcid.org/0000-0002-8587-6153</nameIdentifier>
    </creator>
  </creators>
  <titles>
    <title>Long-term trends and solar cycle response of noctilucent clouds</title>
  </titles>
  <publisher>Universität Rostock</publisher>
  <publicationYear>2024</publicationYear>
  <resourceType resourceTypeGeneral="Text" />
  <subjects>
    <subject xml:lang="en" schemeURI="http://dewey.info/" subjectScheme="dewey">530 Physics</subject>
  </subjects>
  <dates>
    <date dateType="Created">2024</date>
  </dates>
  <language>en</language>
  <alternateIdentifiers>
    <alternateIdentifier alternateIdentifierType="PURL">https://purl.uni-rostock.de/rosdok/id00005166</alternateIdentifier>
    <alternateIdentifier alternateIdentifierType="URN">urn:nbn:de:gbv:28-rosdok_id00005166-6</alternateIdentifier>
  </alternateIdentifiers>
  <descriptions>
    <description descriptionType="Abstract">Noctilucent clouds (NLCs) are ice particle clouds found 80-85 km above Earth's surface in the cold (~130K) summer mesopause region. Their formation requires extremely low temperatures and water vapour (H2O). NLCs are sensitive to temperature and water vapour levels, making them useful tracers for atmospheric conditions in this region. This thesis investigates the 11-year solar cycle's impact on NLCs, water vapor, and temperatures using model simulations, covering 170 years (1849–2019). Results show water vapour response to the solar cycle is altitude-dependent.</description>
  </descriptions>
</resource>
