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Die Hitze in der Stadt verstehen – Wie sich die jahreszeitliche Temperaturdynamik von Städten aus dem All beobachten lässt

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Globale Urbanisierung

Zusammenfassung

Bis zu 95 % der Todesopfer aus Naturkatastrophen sind auf Hitzewellen zurückzuführen. Städte sind außerordentlich betroffen, da sie sich besonders stark erwärmen und hier viele Menschen leben. Die Fernerkundung kann einen Beitrag zu ihrer thermischen Überwachung leisten. Mit Sensoren im Wellenlängenbereich des thermalen Infrarot (TIR) kann beispielsweise die Temperatur der Oberfläche gemessen werden. Neuere Methoden erlauben es mit zahlreichen Aufnahmen über längere Zeiträume genauere thermische Muster abzuleiten und die raumzeitliche Temperaturdynamik städtischer Oberflächen besser zu verstehen. In diesem Kapitel wird der Jahresgang der Oberflächentemperatur und ihrer Wärmeinsel für Städte auf fünf Kontinenten (San Fransisco, Hamburg, Windhoek, Mumbai und Canberra) untersucht.

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Author information

Authors and Affiliations

  1. Centrum für Erdsystemforschung und Nachhaltigkeit, Universität Hamburg, Hamburg, Deutschland

    Benjamin Bechtel Dr.

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  1. Benjamin Bechtel Dr.
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Editors and Affiliations

  1. Georisiken und zivile Sicherheit, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Weßling, Germany

    Hannes Taubenböck

  2. Deutschen Zentrums für Luft- und Raumfahrt (DLR), Weßling, Germany

    Michael Wurm

  3. Dt. Fernerkundungsdatenzentrum Abteilung "GLandoberfläche", Deutsches Zentrum für Luft- und Raumfahrt (DLR), Weßling, Germany

    Thomas Esch

  4. Deutsches Fernerkundungs- datenzentrum (DFD), Deutsches Zentrum für Luft- und Raumfahrt (DLR), Weßling, Germany

    Stefan Dech

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Bechtel, B. (2015). Die Hitze in der Stadt verstehen – Wie sich die jahreszeitliche Temperaturdynamik von Städten aus dem All beobachten lässt. In: Taubenböck, H., Wurm, M., Esch, T., Dech, S. (eds) Globale Urbanisierung. Springer Spektrum, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-44841-0_21

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