Climatic Responses to Future Trans-Arctic Shipping
- Department of Geography, University of Connecticut, Storrs CT USA
- Department of Earth System Science, University of California, Irvine CA USA
- Pacific Northwest National Laboratory, Richland WA USA
As global temperatures increase, sea ice loss will increasingly enable commercial shipping traffic to cross the Arctic Ocean, where the ships' gas and particulate emissions may have strong regional effects. Here we investigate impacts of shipping emissions on Arctic climate using a fully coupled Earth system model (CESM 1.2.2) and a suite of newly developed projections of 21st-century trans-Arctic shipping emissions. We find that trans-Arctic shipping will reduce Arctic warming by nearly 1 °C by 2099, due to sulfate-driven liquid water cloud formation. Cloud fraction and liquid water path exhibit significant positive trends, cooling the lower atmosphere and surface. Positive feedbacks from sea ice growth-induced albedo increases and decreased downwelling longwave radiation due to reduced water vapor content amplify the cooling relative to the shipping-free Arctic. Our findings thus point to the complexity in Arctic climate responses to increased shipping traffic, justifying further study and policy considerations as trade routes open.
- Research Organization:
- Pacific Northwest National Laboratory (PNNL), Richland, WA (United States)
- Sponsoring Organization:
- USDOE
- Grant/Contract Number:
- SC0012998; AC05-76RL01830; AC02-05CH11231; AC05-76RLO1830; NNX14AH55A; 80NSSC17K0540; 80NSSC17K0416
- OSTI ID:
- 1475071
- Alternate ID(s):
- OSTI ID: 1479151; OSTI ID: 1510437
- Report Number(s):
- PNNL-SA-135168
- Journal Information:
- Geophysical Research Letters, Journal Name: Geophysical Research Letters Vol. 45 Journal Issue: 18; ISSN 0094-8276
- Publisher:
- American Geophysical UnionCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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