Vertical Microclimate Stratification
Vertical Microclimate Stratification is a microclimatic phenomenon characterized by the layering of distinct climatic conditions at different heights within a localized environment, distinguished by vertical gradients in temperature, humidity, wind speed, and solar radiation due to differential surface-atmosphere interactions.
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Publications
627
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Authors
33
Institutions
Publications per year
2017–2026
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Fisheries and Oceans Canada
Ottawa, Canada
2 h-index
4 publications
140 citations
Nanjing University
Nanjing, China
1 h-index
1 publications
56 citations
Yuxi Normal University
Yuxi, China
1 h-index
1 publications
33 citations
Universidade de São Paulo
São Paulo, Brazil
1 h-index
6 publications
126 citations

University of Canterbury
Christchurch, New Zealand
1 h-index
1 publications
32 citations

The University of Western Australia
Perth, Australia
1 h-index
1 publications
32 citations
University of Malaya
Kuala Lumpur, Malaysia
1 h-index
1 publications
28 citations
Laboratoire Eau, Environnement et Systèmes Urbains
Champs-sur-Marne, France
1 h-index
1 publications
21 citations
1–8 of 33
1 publications · 32 citations
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1 publications · 25 citations
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1 publications · 24 citations
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1 publications · 33 citations
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1 publications · 32 citations
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