2017
DOI: 10.5670/oceanog.2017.223
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On the Benefit of Current and Future ALPS Data for Improving Arctic Coupled Ocean-Sea Ice State Estimation

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Cited by 20 publications
(27 citation statements)
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“…In contrast to both OSEs and OSSEs, where statistical approach is an important component of the DA step, adjointbased methods utilize the dynamical information in the tangent linear and adjoint models of the underlying general circulation model (GCM). Through the equations which capture conservation and constitutive laws, propagation of information up-and down-stream of any quantity of interest (QoI) is used to (a) assess impactful regions where new observations can be potentially deployed (Marotzke et al, 1999;Zanna et al, 2010;Heimbach et al, 2011;Nguyen et al, 2017;Stammer et al, 2018); (b) assess the redundancy of existing observing networks (Köhl and Stammer, 2004;Moore et al, 2017b); (c) quantify the impacts of selected existing/new observational networks on reducing posterior uncertainties of the GCM control parameters and/or potential unobserved remote QoI (Moore et al, 2011(Moore et al, , 2017aBui-Thanh et al, 2012;Heimbach, 2014, 2018;Kaminski et al, 2015Kaminski et al, , 2018; (d) find an optimal observing network through Hessian-based OED that minimizes the posterior uncertainties as a function of the control parameters and/or targeted QoI (Alexanderian et al, 2016;Loose, 2019). The advantage of the adjoint-based methods is not only the quantification of uncertainty reduction of the GCM control parameters and/or any specific QoI to the observing network but also the identification of dynamical connection and causal relationship between them.…”
Section: System Optimizationmentioning
confidence: 99%
“…In contrast to both OSEs and OSSEs, where statistical approach is an important component of the DA step, adjointbased methods utilize the dynamical information in the tangent linear and adjoint models of the underlying general circulation model (GCM). Through the equations which capture conservation and constitutive laws, propagation of information up-and down-stream of any quantity of interest (QoI) is used to (a) assess impactful regions where new observations can be potentially deployed (Marotzke et al, 1999;Zanna et al, 2010;Heimbach et al, 2011;Nguyen et al, 2017;Stammer et al, 2018); (b) assess the redundancy of existing observing networks (Köhl and Stammer, 2004;Moore et al, 2017b); (c) quantify the impacts of selected existing/new observational networks on reducing posterior uncertainties of the GCM control parameters and/or potential unobserved remote QoI (Moore et al, 2011(Moore et al, , 2017aBui-Thanh et al, 2012;Heimbach, 2014, 2018;Kaminski et al, 2015Kaminski et al, , 2018; (d) find an optimal observing network through Hessian-based OED that minimizes the posterior uncertainties as a function of the control parameters and/or targeted QoI (Alexanderian et al, 2016;Loose, 2019). The advantage of the adjoint-based methods is not only the quantification of uncertainty reduction of the GCM control parameters and/or any specific QoI to the observing network but also the identification of dynamical connection and causal relationship between them.…”
Section: System Optimizationmentioning
confidence: 99%
“…Water and air properties surrounding sea-ice are needed for seaice prediction. Currently, there are no routine observations taken near the edge of sea-ice nor in the transition marginal ice zone (MIZ) between sea ice and open water (Lee et al, 2017;Nguyen et al, 2017). Permanent moored subsurface buoys and ice-tethered profilers could be a key source of time-series data in these data sparse regions.…”
Section: Need For New Observing Technology For S2s Predictionsmentioning
confidence: 99%
“…A display of fields on the native grid, including high latitudes, can be seen in the various references and on the ECCO website. A specific high-northern-latitude version of the state estimate and its corresponding climatology is in preparation (Nguyen et al 2017). Elsewhere, longitudes are uniformly spaced at 1° and latitudes telescope toward the equator (where it is 0.41°) and decrease northward from 1° to about 1/2° at 57°.…”
Section: Basic Fieldsmentioning
confidence: 99%