Observed Mesoscale Hydroclimate Variability of North America’s Allegheny Mountains at 40.2° N
Spatial hydroclimatic variability of Eastern North America’s Allegheny Mountain System (AMS) is commonly oversimplified to elevation differences and the rain-shadow effect. Descriptive and higher order statistical properties of hourly meteorological observations (1948−2017) from...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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MDPI AG
2019-07-01
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| Series: | Climate |
| Subjects: | |
| Online Access: | https://www.mdpi.com/2225-1154/7/7/91 |