Potential Impacts of Winter Arctic Sea Ice on Subsequent Spring Thermal Condition over the Tibetan Plateau
The model results of "Potential Impacts of Winter Arctic Sea Ice on Subsequent Spring Thermal Condition over the Tibetan Plateau". The four seasons are three-month sliding average from preceding December to subsequent May, which is abbreviated as DJF, JFM, FMA, and MAM, respectively.
Main Author: | |
---|---|
Format: | Other/Unknown Material |
Language: | unknown |
Published: |
Zenodo
2024
|
Subjects: | |
Online Access: | https://doi.org/10.5281/zenodo.10775885 |
Summary: | The model results of "Potential Impacts of Winter Arctic Sea Ice on Subsequent Spring Thermal Condition over the Tibetan Plateau". The four seasons are three-month sliding average from preceding December to subsequent May, which is abbreviated as DJF, JFM, FMA, and MAM, respectively. |
---|