The DOI matches its Crossref record; 49 of the 49 references it cites were found in a registry or an index.
High-impact marine heatwaves attributable to human-induced global warming
Abstract
The heat is on: Anthropogenic climate change is causing not only more episodes of historically high air temperatures but also more frequent spells of unusually increased ocean temperatures. Marine heatwaves, defined as periods of anomalously high regional surface ocean temperatures, have also become common in recent decades. Laufkötter et al. show that the frequency of these events has already increased more than 20-fold because of anthropogenic global warming, making marine heatwaves, which typically occurred once in hundreds to thousands of years in preindustrial times, likely to occur on an annual to decadal basis if the global average air temperature rises by 3°C. Science , this issue p. 1621
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Cited by
Surface Modification of 2D Photocatalysts for Solar Energy Conversion
Feng, C., Wu, Z., Huang, K., Ye, J., & Zhang, H. (2022) · Advanced Materials · doi:10.1002/adma.202200180 · Cited by 456
Heat Waves: Physical Understanding and Scientific Challenges
Barriopedro, D., García‐Herrera, R., Ordóñez, C., Miralles, D. G., & Salcedo‐Sanz, S. (2023) · Reviews of Geophysics · doi:10.1029/2022rg000780 · Cited by 404
Propagation of the 2014–2016 Northeast Pacific Marine Heatwave Through the Salish Sea
Khangaonkar, T., Nugraha, A., Yun, S. K., Premathilake, L., Keister, J. E., & Bos, J. (2021) · Frontiers in Marine Science · doi:10.3389/fmars.2021.787604 · Cited by 44
Metadata
- Authors
- Laufkötter, C., Zscheischler, J., & Frölicher, T. L.
- Venue
- Science
- Published
- 2020-09-25
- Volume
- 369
- Issue
- 6511
- Pages
- 1621-1625
- ISSN
- 0036-8075 (ISSN-L)
- 1095-9203
- OpenAlex
- W3089081690
- Cited by
- 470
- References
- 49
- FWCI
- 27.03
- Type
- journal article
- Language
- en
- Open access
- closed
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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