Spatial and temporal variability of the freezing level in Patagonia's atmosphere
<p>The height of the 0 °C isotherm (<span class="inline-formula"><i>H</i><sub>0</sub></span>), which commonly signals the freezing level, denotes the lowest altitude within the atmosphere where the air temperature reaches 0 °C. This can be used as...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-09-01
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| Series: | Weather and Climate Dynamics |
| Online Access: | https://wcd.copernicus.org/articles/5/1137/2024/wcd-5-1137-2024.pdf |