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<front>
<journal-meta>
<journal-id journal-id-type="publisher">GH</journal-id>
<journal-title-group>
<journal-title>Geographica Helvetica</journal-title>
<abbrev-journal-title abbrev-type="publisher">GH</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Geogr. Helv.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2194-8798</issn>
<publisher><publisher-name>Geographisch-Ethnographische Gesellschaft Zürich</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/gh-24-139-1969</article-id>
<title-group>
<article-title>Aarewassertemperatur und Wetter im Mittelland</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kaufmann</surname>
<given-names>P.</given-names>
</name>
</contrib>
</contrib-group><pub-date pub-type="epub">
<day>30</day>
<month>09</month>
<year>1969</year>
</pub-date>
<volume>24</volume>
<issue>3</issue>
<fpage>139</fpage>
<lpage>142</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 1969 P. Kaufmann</copyright-statement>
<copyright-year>1969</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://gh.copernicus.org/articles/24/139/1969/gh-24-139-1969.html">This article is available from https://gh.copernicus.org/articles/24/139/1969/gh-24-139-1969.html</self-uri>
<self-uri xlink:href="https://gh.copernicus.org/articles/24/139/1969/gh-24-139-1969.pdf">The full text article is available as a PDF file from https://gh.copernicus.org/articles/24/139/1969/gh-24-139-1969.pdf</self-uri>
<abstract>
<p>Die statistische Untersuchung des zeitlichen Temperaturablaufs im Aarewasser und in der Luft zeigt,
daß zwischen Fluß- und Lufttemperatur ein eher
loser Zusammenhang besteht, welcher nur während
sommerlicher Schönwetterperioden eine definierte
Form annimmt. Derartige Beziehungen sind im
Landschaftsgefüge nicht selten, worauf kurz hingewiesen wird.</p>
</abstract>
<counts><page-count count="4"/></counts>
</article-meta>
</front>
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<back>
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</article>