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Non-linear motions of Australian geodetic stations induced by non-tidal ocean loading and the passage of tropical cyclones

Non-linear motions of Australian geodetic stations induced by non-tidal ocean loading and the passage of tropical cyclones
Non-linear motions of Australian geodetic stations induced by non-tidal ocean loading and the passage of tropical cyclones
We investigate daily and sub-daily non-tidal oceanic and atmospheric loading (NTOAL) in the Australian region and put an upper bound on potential site motion examining the effects of tropical cyclone Yasi that crossed the Australian coast in January/February 2011. The dynamic nature of the ocean is important, particularly for northern Australia where the long-term scatter due to daily and sub-daily oceanic changes increases by 20–55 % compared to that estimated using the inverted barometer (IB) assumption. Correcting the daily Global Positioning System (GPS) time series for NTOAL employing either a dynamic ocean model or the IB assumption leads to a reduction of up to 52 % in the weighted scatter of daily coordinate estimates. Differences between the approaches are obscured by seasonal variations in the GPS precision along the northern coast. Two compensating signals during the cyclone require modelling at high spatial and temporal resolution: uplift induced by the atmospheric depression, and subsidence induced by storm surge. The latter dominates ( > 135 %) the combined net effect that reaches a maximum of 14 mm, and 10 mm near the closest GPS site TOW2. Here, 96 % of the displacement is reached within 15 h due to the rapid transit of cyclones and the quasi-linear nature of the coastline. Consequently, estimating sub-daily NTOAL is necessary to properly account for such a signal that can be 3.5 times larger than its daily-averaged value. We were unable to detect the deformation signal in 2-hourly GPS processing and show that seasonal noise in the Austral summer dominates and precludes GPS detection of the cyclone-related subsidence.
Non-tidal ocean loading, Storm surge loading, Global positioning system, Australia
0949-7714
927-940
Mémin, A.
ba1c9946-3fbc-44ec-a7bc-1536dbd22ff4
Watson, C.
22fa592a-1fe1-4660-9cdc-825381ce151e
Haigh, I.D.
945ff20a-589c-47b7-b06f-61804367eb2d
MacPherson, L.
2207db66-81a0-485b-8d4e-71c80cc05eb7
Tregoning, P.
44a6ffc6-e5d0-4c64-abdd-d39cb9e0fdc8
Mémin, A.
ba1c9946-3fbc-44ec-a7bc-1536dbd22ff4
Watson, C.
22fa592a-1fe1-4660-9cdc-825381ce151e
Haigh, I.D.
945ff20a-589c-47b7-b06f-61804367eb2d
MacPherson, L.
2207db66-81a0-485b-8d4e-71c80cc05eb7
Tregoning, P.
44a6ffc6-e5d0-4c64-abdd-d39cb9e0fdc8

Mémin, A., Watson, C., Haigh, I.D., MacPherson, L. and Tregoning, P. (2014) Non-linear motions of Australian geodetic stations induced by non-tidal ocean loading and the passage of tropical cyclones. Journal of Geodesy, 88 (10), 927-940. (doi:10.1007/s00190-014-0734-8).

Record type: Article

Abstract

We investigate daily and sub-daily non-tidal oceanic and atmospheric loading (NTOAL) in the Australian region and put an upper bound on potential site motion examining the effects of tropical cyclone Yasi that crossed the Australian coast in January/February 2011. The dynamic nature of the ocean is important, particularly for northern Australia where the long-term scatter due to daily and sub-daily oceanic changes increases by 20–55 % compared to that estimated using the inverted barometer (IB) assumption. Correcting the daily Global Positioning System (GPS) time series for NTOAL employing either a dynamic ocean model or the IB assumption leads to a reduction of up to 52 % in the weighted scatter of daily coordinate estimates. Differences between the approaches are obscured by seasonal variations in the GPS precision along the northern coast. Two compensating signals during the cyclone require modelling at high spatial and temporal resolution: uplift induced by the atmospheric depression, and subsidence induced by storm surge. The latter dominates ( > 135 %) the combined net effect that reaches a maximum of 14 mm, and 10 mm near the closest GPS site TOW2. Here, 96 % of the displacement is reached within 15 h due to the rapid transit of cyclones and the quasi-linear nature of the coastline. Consequently, estimating sub-daily NTOAL is necessary to properly account for such a signal that can be 3.5 times larger than its daily-averaged value. We were unable to detect the deformation signal in 2-hourly GPS processing and show that seasonal noise in the Austral summer dominates and precludes GPS detection of the cyclone-related subsidence.

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More information

Published date: October 2014
Keywords: Non-tidal ocean loading, Storm surge loading, Global positioning system, Australia
Organisations: Physical Oceanography

Identifiers

Local EPrints ID: 370266
URI: http://eprints.soton.ac.uk/id/eprint/370266
ISSN: 0949-7714
PURE UUID: 5393770c-1335-4f72-9690-e1ef496057b1
ORCID for I.D. Haigh: ORCID iD orcid.org/0000-0002-9722-3061

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Date deposited: 20 Oct 2014 15:33
Last modified: 15 Mar 2024 03:26

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Contributors

Author: A. Mémin
Author: C. Watson
Author: I.D. Haigh ORCID iD
Author: L. MacPherson
Author: P. Tregoning

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