Mooring and Seafloor Pressure End Point Measurements at the Southern Entrance of the Solomon Sea: Subseasonal to Interannual Flow Variability
Abstract
Variability of the flow across the Solomon Sea's southern entrance was examined using end point subsurface moorings and seafloor pressure sensors, reconstructed velocity profiles based on satellite-derived surface velocity and bottom pressure-derived subsurface velocity, and 1993–2017 proxy volume transport based on satellite altimetry. The reconstructed velocity correctly represents the fluctuating surface flow and subsurface core providing a high-frequency continuous observing system for this sea. The mean equatorward volume transport over 0- to 500-m depth layer is 15.2 Sv (1 Sv ≡ 106 m3/s) during July 2012 to May 2017. The measurements resolve the full spectrum of the volume transport including energetic subseasonal variability that fluctuates by as much as 25 Sv over one week. At low-frequency timescales, the study finds that linear Rossby waves forced by Ekman pumping in the interior of the Pacific influence not only seasonal fluctuations as found by previous studies but also interannual variability. As found previously, the El Niño–Southern Oscillation highly influences interannual volume transport. During the 2015/2016 El Niño, observations show the seasonal cycle to be suppressed from the second half of 2014, prior to the mature phase of the El Niño, to September 2016 along with an increase in across-transect transport. At subseasonalmore »
- Authors:
-
- Scripps Inst. of Oceanography, La Jolla, CA (United States)
- Publication Date:
- Research Org.:
- Univ. of California, San Diego, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC); National Science Foundation (NSF); National Oceanic and Atmospheric Administration (NOAA); National Aeronautics and Space Administration (NASA)
- OSTI Identifier:
- 1611947
- Alternate Identifier(s):
- OSTI ID: 1544440
- Grant/Contract Number:
- SC0012778; NA15OAR4320071; 80NSSC17K0373; OCE1029487
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Journal of Geophysical Research. Oceans
- Additional Journal Information:
- Journal Volume: 124; Journal Issue: 7; Journal ID: ISSN 2169-9275
- Publisher:
- American Geophysical Union
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; oceanography; Solomon Sea; NGCC; NGCU
Citation Formats
Anutaliya, Arachaporn, Send, Uwe, Sprintall, Janet, McClean, Julie L., Lankhorst, Matthias, and Koelling, Jannes. Mooring and Seafloor Pressure End Point Measurements at the Southern Entrance of the Solomon Sea: Subseasonal to Interannual Flow Variability. United States: N. p., 2019.
Web. doi:10.1029/2019jc015157.
Anutaliya, Arachaporn, Send, Uwe, Sprintall, Janet, McClean, Julie L., Lankhorst, Matthias, & Koelling, Jannes. Mooring and Seafloor Pressure End Point Measurements at the Southern Entrance of the Solomon Sea: Subseasonal to Interannual Flow Variability. United States. https://doi.org/10.1029/2019jc015157
Anutaliya, Arachaporn, Send, Uwe, Sprintall, Janet, McClean, Julie L., Lankhorst, Matthias, and Koelling, Jannes. Sat .
"Mooring and Seafloor Pressure End Point Measurements at the Southern Entrance of the Solomon Sea: Subseasonal to Interannual Flow Variability". United States. https://doi.org/10.1029/2019jc015157. https://www.osti.gov/servlets/purl/1611947.
@article{osti_1611947,
title = {Mooring and Seafloor Pressure End Point Measurements at the Southern Entrance of the Solomon Sea: Subseasonal to Interannual Flow Variability},
author = {Anutaliya, Arachaporn and Send, Uwe and Sprintall, Janet and McClean, Julie L. and Lankhorst, Matthias and Koelling, Jannes},
abstractNote = {Variability of the flow across the Solomon Sea's southern entrance was examined using end point subsurface moorings and seafloor pressure sensors, reconstructed velocity profiles based on satellite-derived surface velocity and bottom pressure-derived subsurface velocity, and 1993–2017 proxy volume transport based on satellite altimetry. The reconstructed velocity correctly represents the fluctuating surface flow and subsurface core providing a high-frequency continuous observing system for this sea. The mean equatorward volume transport over 0- to 500-m depth layer is 15.2 Sv (1 Sv ≡ 106 m3/s) during July 2012 to May 2017. The measurements resolve the full spectrum of the volume transport including energetic subseasonal variability that fluctuates by as much as 25 Sv over one week. At low-frequency timescales, the study finds that linear Rossby waves forced by Ekman pumping in the interior of the Pacific influence not only seasonal fluctuations as found by previous studies but also interannual variability. As found previously, the El Niño–Southern Oscillation highly influences interannual volume transport. During the 2015/2016 El Niño, observations show the seasonal cycle to be suppressed from the second half of 2014, prior to the mature phase of the El Niño, to September 2016 along with an increase in across-transect transport. At subseasonal timescales, local Ekman pumping and remote wind stress curl are responsible for a third of the subseasonal variance. Finally, the study highlights the importance of high-frequency observations at the southern entrance of the Solomon Sea and the ability of a linear Rossby model to represent the low-frequency variability of the transport.},
doi = {10.1029/2019jc015157},
journal = {Journal of Geophysical Research. Oceans},
number = 7,
volume = 124,
place = {United States},
year = {Sat Jul 06 00:00:00 EDT 2019},
month = {Sat Jul 06 00:00:00 EDT 2019}
}
Web of Science
Figures / Tables:
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