A principal goal of this project is to quantitatively assess the spatial characteristics of the strain response of the Ross Ice Shelf (RIS) to the ocean gravity wave spectrum through an annual cycle. Changes in the ocean environment due to a changing climate (e.g., increasing storminess, decreasing sea-ice cover, and warming ocean waters) would affect the integrity of West Antarctica’s ice shelves. The response of the RIS depends on properties of the coupled ice shelf/sub-ice shelf water cavity system underlain by the solid Earth, as well as on the structural and elastic properties of the ice and their variability. Environmentally induced changes in the ice-shelf system can be detected using seismometers deployed on the ice-shelf, e.g. by observing changes in RIS resonance characteristics (Bromirski and Stephen, 2012) or changes in the cross-correlation between sensors (Shapiro et al., 2005, Gerstoft et al., 2006) of seismic noise or wave impact signals .
This study was motivated by initial analysis of broadband seismometer data collected near the front of the Ross Ice Shelf during 2005-2006 by Cathles et al. (2009) and MacAyeal et al. (2006).
Ice shelves buttress ice sheets on land, restraining ice sheet movement towards the ocean. Ice shelves are appreciably (and constantly), flexed, rocked, rolled, pitched, elongated and compressed by various components of ocean waves. Recent theory and observations indicate that a better understanding of ice-shelf/ocean-wave interactions can lead to a better understanding of ice-shelf evolution in a changing environment, that includes increased storminess and related ocean-wave effects (Bromirski et al., 2005a; Bromirski et al., 2003). Gravity wave impacts could significantly affect ice shelf rift propagation, expansion of crevasses and other pre-existing fractures, affecting ice shelf integrity. The collapse of ice shelves allows glacial ice on land to flow faster to the ocean, raising sea level. The response of ice shelves to gravity wave impacts and ice shelf properties can be measured by seismometers deployed on ice shelves.
Ocean waves impacting the Ross Ice Shelf originate in the North Pacific (e.g. path c in Figure 1) as well as in the Southern Ocean surrounding Antarctica (Cathes et al., 2009; Bromirski et al., 2010). North Pacific swell (10-30s period) is transformed along coasts to very long period (50-300s) infragravity (IG) waves (Herbers et al. 1995). Some of the coastally-trapped IG wave energy leaks off the North American continental shelf and propagates to Antarctica along paths a and b. Ice shelves respond to wave impacts at characteristic frequencies, depending on ice shelf thickness and water depth below the floating shelf (Bromirski and Stephen, 2012).
Spectral characteristics (Figure 2) of the response of the RIS to gravity wave impacts (recorded by a seismometer at N) allow determination of their generation location. The wave impact signal at the RIS from the extreme North Pacific wave event (path c in Fig. 1; circled in black in Fig. 2) occurs during the Antarctic summer, when sea ice (that damps ocean wave energy) is at a minimum. The sea ice damping effect (exhibited by the much lower spectral levels within the white circled region in Fig. 2) is most pronounced during the Antarctic winter when Southern ocean storms are strongest. So North Pacific waves may have a greater impact on the RIS than waves generated locally.
References & Further Information
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Response of the Ross Ice Shelf to gravity wave forcing,
Ann. Glaciol., 53(60), doi:10.3189/2012AoG60A058.
Bromirski, P.D., O.V. Sergienko, D.R. MacAyeal (2010).
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Bromirski, P.D., F. K. Duennebier and R. A. Stephen (2005).
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