The impact of changes in tropical sea surface temperatures over 1979–2012 on northern hemisphere high-latitude climate

McCrystall, Michelle R.; Hosking, J. Scott ORCID:; White, Ian P.; Maycock, Amanda C.. 2020 The impact of changes in tropical sea surface temperatures over 1979–2012 on northern hemisphere high-latitude climate. Journal of Climate, 33 (12). 5103-5121.

Before downloading, please read NORA policies.
© 2020 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (
jcli-d-19-0456.1.pdf - Published Version

Download (3MB) | Preview


While rapid changes in Arctic climate over recent decades are widely documented, the importance of different driving mechanisms is still debated. A previous study proposed a causal connection between recent tropical Pacific sea surface temperature (SST) trends and circulation changes over northern Canada and Greenland (NCG). Here, using the HadGEM3-A model, we perform a suite of sensitivity experiments to investigate the influence of tropical SSTs on winter atmospheric circulation over NCG. The experiments are forced with observed SST changes between an “early” (1979–88) and “late” period (2003–12) and applied across the entire tropics (TropSST), the tropical Pacific (PacSST), and the tropical Atlantic (AtlSST). In contrast to the previous study, all three experiments show a negative 200-hPa eddy geopotential height (Z200) anomaly over NCG in winter, which is similar to the response in AMIP experiments from four other climate models. The positive Z200 NCG anomaly in ERA-Interim between the two periods is inside the bounds of internal variability estimated from bootstrap sampling. The NCG circulation anomaly in the TropSST experiment is associated with a Rossby wave train originating from the tropical Pacific, with an important contribution coming from the tropical Atlantic SSTs connected via an atmospheric bridge through the tropical Pacific. This generates anomalous upper-level convergence and a positive Rossby wave source anomaly near the North Pacific jet exit region. Hence, while a tropics–Arctic teleconnection is evident, its influence on recent Arctic regional climate differs from observed changes and warrants further research.

Item Type: Publication - Article
Digital Object Identifier (DOI):
ISSN: 0894-8755
Additional Keywords: Arctic; Tropics; Rossby waves; Teleconnections; Walker circulation
Date made live: 28 May 2020 11:14 +0 (UTC)

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...