Is the Upper Ocean Warming? Comparisons of 50-Year Trends from Different Analyses*
Abstract
There is great interest in World Ocean temperature trends, yet the historical global ocean database has very uneven coverage in space and time. Previous work on 50-yr upper ocean temperature trends from the NOAA ocean data archive is extended here. Trends at depths from 50 to 1000 m are examined, based on observations gridded over larger regions than in the earlier study. Despite the use of larger grid boxes, most of the ocean does not have significant 50-yr trends at the 90% confidence level (CL). In fact only 30% of the ocean at 50 m has 90% CL trends, and the percentage decreases significantly with increasing depth. As noted in the previous study, there is much spatial structure in 50-yr trends, with areas of strong warming and strong cooling. These trend results are compared with trends calculated from data interpolated to standard levels and from a highly horizontally interpolated version of the dataset that has been used in previous heat content trend studies. The regional trend results can differ substantially, even in the areas with statistically significant trends. Trends based on the more interpolated analyses show more warming. Together with major temporal and spatial sampling limitations, the previously described strong interdecadal and spatial variability of trends makes it very difficult to formally estimate uncertainty in World Ocean averages, but these results suggest that upper ocean heat content integrals and integral trends may be substantially more uncerta…
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Carson and Harrison (2008) found that the upper 300 m of the Canary upwelling system have been subject to warming from 1955 to 2003.
“According to Carson and Harrison (2008), the upper 300 m of the Canary upwelling system have been subject to warming from 1955 to 2003.”
From Recent Trends in SST, Chl‐<i>a</i>, Productivity and Wind Stress in Upwelling and Open Ocean Areas in the Upper Eastern North Atlantic Subtropical Gyre (2021) · cites this paper as Carson and Harrison (2008)
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Canary current upwelling: More or less?
Barton, E. D., Field, D. B., & Roy, C. (2013) · Progress in Oceanography · doi:10.1016/j.pocean.2013.07.007 · Cited by 134 · see citing works
Siemer, J. P., Machín, F., González‐Vega, A., Arrieta, J. M., Gutiérrez‐Guerra, M. A., Pérez‐Hernández, M. D., Vélez‐Belchí, P., Hernández‐Guerra, A., & Fraile‐Nuez, E. (2021) · Journal of Geophysical Research: Oceans · doi:10.1029/2021jc017268 · Cited by 50 · see citing works
- Authors
- Carson, M., & Harrison, D. E.
- Affiliations
- University of Washington (US)
- National Oceanic and Atmospheric Administration (US)
- Corresponding author
- Carson, Mark
- ORCID
- Carson, Mark
- Venue
- Journal of Climate
- Publisher
- American Meteorological Society
- Published
- 2008-05-15
- Volume
- 21
- Issue
- 10
- Pages
- 2259-2268
- ISSN
- 0894-8755 (ISSN-L)
- 1520-0442
- OpenAlex
- W2082218014
- Cited by
- 13
- References
- 0
- Citations by year
- 2024: 2 · 2023: 1 · 2021: 1 · 2016: 1 · 2015: 1 · 2013: 1 · 2012: 3
- FWCI
- 0.70
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Climate (publishedVersion)
- Funders
- Joint Institute for the Study of the Atmosphere and Ocean
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Keywords
- upper ocean warming, ocean temperature trends, ocean heat content, interannual variability, data interpolation
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