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Title: 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 » 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.« less

Authors:
ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [1]; ORCiD logo [1]
  1. 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}
}

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Figures / Tables:

Figure 1 Figure 1: Bathymetry of the Solomon Sea and its surroundings along with the location of the moorings and PIES (magenta triangles) near Misima (M) and Gizo (G) Islands. Schematic of dominant Solomon Sea currents are represented by the gray arrows; NGCC is New Guinea Coastal Current, NGCU is New Guineamore » Coastal Undercurrent, GPC is Gulf of Papua Current, NVJ is North Vanuatu Jet, EUC is Equatorial Undercurrent, SEC is South Equatorial Current, SECC is South Equatorial Countercurrent. Black contours are plotted for 0‐ and 1,000‐m depth. The inset shows locations used to construct the proxy volume transport (maroon crosses) and Δh (green circles).« less

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