Future Changes in the Free Tropospheric Freezing Level and Rain–Snow Limit: The Case of Central Chile
The freezing level in the free troposphere often intercepts the terrain of the world’s major mountain ranges, creating a rain–snow limit. In this work, we use the free tropospheric height of the 0 <inline-formula><math display="inline"><semantics><msup><mrow>&...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
MDPI AG
2020-11-01
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| Series: | Atmosphere |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2073-4433/11/11/1259 |