Feature Publication Archive
Johnson, G.C. (2017): Overview. In State of the Climate in 2016, Global Oceans. Bull. Am. Meteorol. Soc., 98 (8), S63
Johnson, G.C., J.M. Lyman, T. Boyer, C.M. Domingues, J. Gilson, M. Ishii, R. Killick, D. Monselan, and S. Wijffels (2017): Ocean heat content. In State of the Climate in 2016, Global Oceans. Bull. Am. Meteorol. Soc., 98 (8), S66–S69
Johnson, G.C., J. Reagan, J.M. Lyman, T. Boyer, C. Schmid, and R. Locarnini (2017): Salinity. In State of the Climate in 2016, Global Oceans. Bull. Am. Meteorol. Soc., 98 (8), S69–S75
Feely, R.A., R. Wanninkhof, P. Landschützer, B.R. Carter, and J.A. Triñanes (2017): Ocean carbon. In State of the Climate in 2016, Global Oceans. Bull. Am. Meteorol. Soc., 98 (8), S89–S92.
Overland, J., E. Hanna, I. Hanssen-Bauer, S.-J. Kim, J.E. Walsh, M. Wang, U.S. Bhatt, and R.L. Thoman (2017): Arctic air temperature. In State of the Climate in 2016, The Arctic. Bull. Am. Meteorol. Soc., 98 (8), S130–S131.
NOAA has led, for 27 years, a team of international scientists in issuing annual reports on the state of the climate focusing on the year just passed. The State of the Climate in 2016 report, published as a supplement to Bulletin of the American Meteorological Society in August 2017, is the most recent release of this report. Seven Federal, JISAO (Joint Institute for the Study of the Atmosphere and Ocean, University of Washington), and JIMAR (Joint Institute for Marine and Atmospheric Research, University of Hawaii) scientists resident at PMEL co-authored four of twelve sections in the... more »
McClatchie, S., A. R. Thompson, S. R. Alin, S. Siedlecki, W. Watson, and S. J. Bograd (2016), The influence of Pacific Equatorial Water on fish diversity in the southern California Current System,J. Geophys. Res. Oceans, 121, doi:10.1002/2016JC011672.
Changes in large-scale ocean circulation due to climate change appear to be underway throughout the world ocean and stand to significantly affect marine ecosystems and resources. This new study by McClatchie et al. investigated whether changes in the character of coastal waters over the last 30 years have affected the composition of fish communities in the southern California Current ecosystem. The California Undercurrent transports Pacific Equatorial Water into the Southern California Bight from... more »
Every year NOAA leads a team of international scientists in issuing a report on the state of the climate in the year just passed, published as a supplement to Bulletin of the American Meteorological Society. Nine Federal, JISAO, and JIMAR scientists resident at PMEL co-authored four of twelve sections in the Global Oceans chapter and one section in the Arctic chapter for the State of the Climate in 2015 report, published in July 2016. In addition, Dr. Gregory Johnson served as lead editor of the Global Oceans chapter and participated in the media roll-out event.
Dr. Johnson’s... more »
Composite evolution of extreme El Niño events in WWBs (contours) and anomalous temperature (colors). One WWB early in the year warms the central Pacific making additional WWBs more likely. Many WWBs are necessary to trigger an extreme El Niño event.
Levine, A.F.Z., F.-F. Jin, and M.J. McPhaden (2016): Extreme noise–extreme El Niño: How state-dependent noise forcing creates El Niño-La Niña asymmetry. J. Climate, doi:10.1175/JCLI-D-16-0091.1
Published online. http://journals.ametsoc.org/doi/10.1175/JCLI-D-16-0091.1
A major unanswered question about El Niño-Southern Oscillation (ENSO) is why the largest El Niño events are stronger in magnitude than the largest La Niña events. This paper examines one of the leading hypotheses to explain this asymmetric behavior; namely, that westerly wind bursts (WWBs) create conditions to promote additional WWBs, and the sum total of all the WWBs that occur during the initiation and growth of an El Niño event impacts the eventual magnitude of the event. WWBs are short episodic bursts of westerly winds that occur in the opposite direction of the normal trade winds.... more »
A comparison of the 2015 and 1997 El Niños. Credit: NASA’s Earth Observatory.
Levine, A. F. Z., and M. J. McPhaden (2016), How the July 2014 Easterly Wind Burst Gave the 2015-6 El Niño a Head Start, Geophys. Res. Lett., 43, doi:10.1002/2016GL069204.
Following strong westerly wind bursts in boreal winter and spring of 2014, both the scientific community and the popular press were abuzz with the possibility of a major El Niño developing, but the widely anticipated major 2014-5 El Niño event didn't even qualify as an El Niño by conventional definitions.
The boreal summer easterly wind burst inhibited the growth of the El Niño event, and also prevented and then reversed the discharge of the equatorial heat content that typically occurs during the course of an El Niño event. This head start of equatorial heat content helped push the... more »