Polar Day
Polar Day is a geophysical phenomenon characterized by the continuous presence of daylight at a planetary pole during its hemisphere's summer solstice, resulting from the planet's axial tilt and orbital position around the Sun.
42
Publications
1.6K
Citations
220
Authors
84
Institutions
Publications per year
2017–2026
14
Variants
Midnight Sun
Parents
42
Manfred Wendisch, Andreas Macke, André Ehrlich et al. · Bulletin of the American Meteorological Society · 2018 · 454 citations · Full text
André Ehrlich, Manfred Wendisch, Christof Lüpkes et al. · Earth system science data · 2019 · 88 citations · Full text
1–5 of 42
220
4
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3
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3
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Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Germany
3 publications · 638 citations
3
h-index
3
h-index
1–5 of 220
84
Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
Bremerhaven, Germany
5 h-index
24 publications
5.6K citations
University of Bremen
Bremen, Germany
4 h-index
11 publications
3.8K citations
Norwegian Institute for Nature Research
Trondheim, Norway
4 h-index
6 publications
351 citations

University of Cologne
Cologne, Germany
4 h-index
13 publications
2.8K citations
Leibniz Institute for Tropospheric Research
Leipzig, Germany
3 h-index
26 publications
10.4K citations
Johannes Gutenberg University Mainz
Mainz, Germany
3 h-index
7 publications
1.7K citations
Leipzig University
Leipzig, Germany
3 h-index
19 publications
6.1K citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
13 publications
3.1K citations
1–8 of 84
JGR · 3 publications · 99 citations
3
h-index
3 publications · 133 citations
3
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Repository · 3 publications · 56 citations
3
h-index
2 publications · 78 citations
2
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2 publications · 42 citations
2
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1–5