Vertical mixing and coral death in the Red Sea following the eruption of Mount Pinatubo
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Due to the weak stratification of the water column in the northern part of the basin, the convective mixing can be especially deep and reaches the sea floor.
“Due to the weak stratification of the water column in the northern part of the basin, the convective mixing can be especially deep and reaches the sea floor42,44,45.”
From The Red Sea Deep Water is a potent source of atmospheric ethane and propane (2020) · cites this paper as [44]
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- Authors
- Genin, A., Lazar, B., & Brenner, S.
- Affiliations
- Hebrew University of Jerusalem (IL)
- Israel Oceanographic and Limnological Research (IL)
- ORCID
- Genin, Amatzia
- Venue
- Nature
- Published
- 1995-10
- Volume
- 377
- Issue
- 6549
- Pages
- 507-510
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W1993966444
- Cited by
- 313
- References
- 26
- Citations by year
- 2026: 5 · 2025: 12 · 2024: 6 · 2023: 7 · 2022: 10 · 2021: 19 · 2020: 13 · 2019: 6 · 2018: 12 · 2017: 11 · 2016: 7 · 2015: 7 · 2014: 6 · 2013: 13 · 2012: 7
- FWCI
- 11.50
- Type
- journal article
- Language
- en
- Open access
- closed
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Nature (publishedVersion)
- Oceanographic literature review
- Topics
- Physical Sciences › Environmental Science › Ecology › Coral and Marine Ecosystems Studies
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Keywords
- Mount Pinatubo eruption, vertical mixing, Gulf of Aqaba, Red Sea, phytoplankton blooms, filamentous algae, water column stratification, air-sea heat flux, atmospheric cooling, coral reefs, fossil reefs, paleoclimate indicators
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