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Title: Climatic Responses to Future Trans-Arctic Shipping

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2018GL078969· OSTI ID:1475071

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
Citation Metrics:
Cited by: 27 works
Citation information provided by
Web of Science

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