Amplified Arctic warming by phytoplankton under greenhouse warming
One of the important impacts of marine phytoplankton on climate systems is the geophysical feedback by which chlorophyll and the related pigments in phytoplankton absorb solar radiation and then change sea surface temperature. Yet such biogeophysical impact is still not considered in many climate pr...
| Published in: | Proceedings of the National Academy of Sciences |
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| Main Authors: | , , , , |
| Format: | Text |
| Language: | English |
| Published: |
National Academy of Sciences
2015
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| Subjects: | |
| Online Access: | http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4434777/ http://www.ncbi.nlm.nih.gov/pubmed/25902494 https://doi.org/10.1073/pnas.1416884112 |
| Summary: | One of the important impacts of marine phytoplankton on climate systems is the geophysical feedback by which chlorophyll and the related pigments in phytoplankton absorb solar radiation and then change sea surface temperature. Yet such biogeophysical impact is still not considered in many climate projections by state-of-the-art climate models, nor is its impact on the future climate quantified. This study shows that, by conducting global warming simulations with and without an active marine ecosystem model, the biogeophysical effect of future phytoplankton changes amplifies Arctic warming by 20%. Given the close linkage between the Arctic and global climate, the biologically enhanced Arctic warming can significantly modify future estimates of global climate change, and therefore it needs to be considered as a possible future scenario. |
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