Super-Clausius–Clapeyron scaling of extreme precipitation explained by shift from stratiform to convective rain type.
Tools
Tools
Tools
Da Silva, Nicolas A. 
ORCID: https://orcid.org/0000-0003-3255-9274 and Haerter, Jan O. ORCID: https://orcid.org/0000-0002-8617-3847
(2025)
Super-Clausius–Clapeyron scaling of extreme precipitation explained by shift from stratiform to convective rain type.
Nature Geoscience
.
DOI https://doi.org/10.1038/s41561-025-01686-4.
![[img]](http://cris.leibniz-zmt.de/style/images/fileicons/text.png) |
Text
Haerter.pdf - Published Version Available under License Creative Commons: Attribution 4.0. Download (5MB) |
Official URL: http://dx.doi.org/10.1038/s41561-025-01686-4
| Document Type: | Article |
|---|---|
| Programme Area: | PA2 |
| Research affiliation: | Integrated Modelling > Complexity and Climate |
| Refereed: | Yes |
| Open Access Journal?: | No |
| DOI: | https://doi.org/10.1038/s41561-025-01686-4 |
| ISSN: | 1752-0894 |
| Date Deposited: | 12 May 2025 16:16 |
| Last Modified: | 12 May 2025 16:16 |
| URI: | http://cris.leibniz-zmt.de/id/eprint/5657 |
Actions (login required)
 |
View Item |