Amplification of global warming through pH dependence of DMS production simulated with a fully coupled Earth system model
We estimate the additional transient surface warming Δ<i>T</i><sub>s</sub> caused by a potential reduction of marine dimethyl sulfide (DMS) production due to ocean acidification under the high-emission scenario RCP8.5 until the year 2200. Since we use a fully coupled Earth...
| Main Authors: | , , , , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2017-08-01
|
| Series: | Biogeosciences |
| Online Access: | https://www.biogeosciences.net/14/3633/2017/bg-14-3633-2017.pdf |