Vertical, horizontal, and temporal changes in temperature in the Atlantis II and Discovery hot brine pools, Red Sea

Handle URI:
http://hdl.handle.net/10754/600167
Title:
Vertical, horizontal, and temporal changes in temperature in the Atlantis II and Discovery hot brine pools, Red Sea
Authors:
Swift, Stephen A.; Bower, Amy S.; Schmitt, Raymond W.
Abstract:
In October 2008, we measured temperature and salinity in hot, hypersaline brine filling the Atlantis II and Discovery Deeps on the Red Sea spreading center west of Jeddah, Saudi Arabia. In agreement with previous observations in the Atlantis II Deep, we found a stack of four convective layers with vertically uniform temperature profiles separated by thin interfaces with high vertical temperature gradients. Temperature in the thick lower convective layer in the Atlantis II Deep continued to slowly increase at 0.1 °C/year since the last observations in 1997. Previously published data show that the temperature of all four convective layers increased since the 1960s at the same rate, from which we infer that diffusive vertical heat flux between convective layers is rapid on time scales of 3-5 years and, thus, heat is lost from the brine pools to overlying Red Sea Deep Water. Heat budgets suggest that the heat flux from hydrothermal venting has decreased from 0.54. GW to 0.18. GW since 1966. A tow-yo survey found that temperature in the upper convective layers changes about 0.2 °C over 5-6. km but the temperature in the lower brine layer remains constant. Temperature in the lower convective layer in the Discovery Deep remains unchanged at 48 °C. To explain these results, we hypothesize that heat flux from a hydrothermal vent in the floor of the Discovery Deep has been stable for 40 years, whereas temperature of the brine in the Atlantis II Deep is adjusting to the change in hydrothermal heat flux from the vent in the Southwest Basin. We found no changes in the upper transition layer at 1900-1990. m depth that appeared between 1976 and 1992 and suggest that this layer originated from the seafloor elsewhere in the rift. © 2012 Elsevier Ltd.
Citation:
Swift SA, Bower AS, Schmitt RW (2012) Vertical, horizontal, and temporal changes in temperature in the Atlantis II and Discovery hot brine pools, Red Sea. Deep Sea Research Part I: Oceanographic Research Papers 64: 118–128. Available: http://dx.doi.org/10.1016/j.dsr.2012.02.006.
Publisher:
Elsevier BV
Journal:
Deep Sea Research Part I: Oceanographic Research Papers
KAUST Grant Number:
USA 00002; KSA 00011; KSA 00011/02
Issue Date:
Jun-2012
DOI:
10.1016/j.dsr.2012.02.006
Type:
Article
ISSN:
0967-0637
Sponsors:
We gratefully acknowledge the financial and logistical support for the R/V Oceanus cruise provided by King Abdullah University of Science and Technology (KAUST), as well as the support of an international group of scientists and technicians during the cruise. This research is based on work supported by Award Nos. USA 00002, KSA 00011 and KSA 00011/02 made by KAUST. Guidance and support in Saudi Arabia was provided by Y. Kattan, A. Al-Suwailem, H. Al-Jandali, and J. Luyten. In the US, ship operations were facilitated by L. Madin, R. Detrick, A. Suchy, L. Capporelli, K. Heywood and B. Costello. We thank the officers and crew of the R/V Oceanus for their assistance at-sea. Instrument operations and data acquisition were ably managed by F. Bahr, M. Swartz, and G. Tupper (WHOI). G. Tupper also did the oxygen and salinity analyses and managed operation of the Hobo sensors. We are very grateful to M. Swartz, who calibrated the Hobos, and to T. McKee, who processed the CTD data and applied corrections for bottle analyses to salinity and oxygen results. Lars-Goran Danielsson kindly provided hydrographic data for the 1976 survey of the R/V Akademik Kurchatouv that appeared in figures of Bubnov et al. (1977). We thank an anonymous reviewer for corrections and helpful suggestions on the manuscript.
Appears in Collections:
Publications Acknowledging KAUST Support

Full metadata record

DC FieldValue Language
dc.contributor.authorSwift, Stephen A.en
dc.contributor.authorBower, Amy S.en
dc.contributor.authorSchmitt, Raymond W.en
dc.date.accessioned2016-02-28T06:44:12Zen
dc.date.available2016-02-28T06:44:12Zen
dc.date.issued2012-06en
dc.identifier.citationSwift SA, Bower AS, Schmitt RW (2012) Vertical, horizontal, and temporal changes in temperature in the Atlantis II and Discovery hot brine pools, Red Sea. Deep Sea Research Part I: Oceanographic Research Papers 64: 118–128. Available: http://dx.doi.org/10.1016/j.dsr.2012.02.006.en
dc.identifier.issn0967-0637en
dc.identifier.doi10.1016/j.dsr.2012.02.006en
dc.identifier.urihttp://hdl.handle.net/10754/600167en
dc.description.abstractIn October 2008, we measured temperature and salinity in hot, hypersaline brine filling the Atlantis II and Discovery Deeps on the Red Sea spreading center west of Jeddah, Saudi Arabia. In agreement with previous observations in the Atlantis II Deep, we found a stack of four convective layers with vertically uniform temperature profiles separated by thin interfaces with high vertical temperature gradients. Temperature in the thick lower convective layer in the Atlantis II Deep continued to slowly increase at 0.1 °C/year since the last observations in 1997. Previously published data show that the temperature of all four convective layers increased since the 1960s at the same rate, from which we infer that diffusive vertical heat flux between convective layers is rapid on time scales of 3-5 years and, thus, heat is lost from the brine pools to overlying Red Sea Deep Water. Heat budgets suggest that the heat flux from hydrothermal venting has decreased from 0.54. GW to 0.18. GW since 1966. A tow-yo survey found that temperature in the upper convective layers changes about 0.2 °C over 5-6. km but the temperature in the lower brine layer remains constant. Temperature in the lower convective layer in the Discovery Deep remains unchanged at 48 °C. To explain these results, we hypothesize that heat flux from a hydrothermal vent in the floor of the Discovery Deep has been stable for 40 years, whereas temperature of the brine in the Atlantis II Deep is adjusting to the change in hydrothermal heat flux from the vent in the Southwest Basin. We found no changes in the upper transition layer at 1900-1990. m depth that appeared between 1976 and 1992 and suggest that this layer originated from the seafloor elsewhere in the rift. © 2012 Elsevier Ltd.en
dc.description.sponsorshipWe gratefully acknowledge the financial and logistical support for the R/V Oceanus cruise provided by King Abdullah University of Science and Technology (KAUST), as well as the support of an international group of scientists and technicians during the cruise. This research is based on work supported by Award Nos. USA 00002, KSA 00011 and KSA 00011/02 made by KAUST. Guidance and support in Saudi Arabia was provided by Y. Kattan, A. Al-Suwailem, H. Al-Jandali, and J. Luyten. In the US, ship operations were facilitated by L. Madin, R. Detrick, A. Suchy, L. Capporelli, K. Heywood and B. Costello. We thank the officers and crew of the R/V Oceanus for their assistance at-sea. Instrument operations and data acquisition were ably managed by F. Bahr, M. Swartz, and G. Tupper (WHOI). G. Tupper also did the oxygen and salinity analyses and managed operation of the Hobo sensors. We are very grateful to M. Swartz, who calibrated the Hobos, and to T. McKee, who processed the CTD data and applied corrections for bottle analyses to salinity and oxygen results. Lars-Goran Danielsson kindly provided hydrographic data for the 1976 survey of the R/V Akademik Kurchatouv that appeared in figures of Bubnov et al. (1977). We thank an anonymous reviewer for corrections and helpful suggestions on the manuscript.en
dc.publisherElsevier BVen
dc.subjectAtlantis II Deepen
dc.subjectBrine poolsen
dc.subjectDiscovery Deepen
dc.subjectHydrothermal venten
dc.subjectRed Seaen
dc.titleVertical, horizontal, and temporal changes in temperature in the Atlantis II and Discovery hot brine pools, Red Seaen
dc.typeArticleen
dc.identifier.journalDeep Sea Research Part I: Oceanographic Research Papersen
dc.contributor.institutionWoods Hole Oceanographic Institution, Woods Hole, United Statesen
kaust.grant.numberUSA 00002en
kaust.grant.numberKSA 00011en
kaust.grant.numberKSA 00011/02en
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