2019
DOI: 10.1016/j.dynatmoce.2019.101107
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Characteristics and evolution of a coastal mesoscale eddy in the Western Bay of Bengal monitored by high-frequency radars

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Cited by 28 publications
(13 citation statements)
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“…In addition, the highly dynamic nature and the role of multiple factors affecting SSTs make it difficult to explore these relationships, if any. Some of the factors affecting SSTs are solar insolation, warm/cold water advection, and other marine processes, namely ocean currents, upwelling/downwelling phenomena, and eddies (Leeuwenburgh and Stammer, 2001;Shinoda, 2005;Krishna, 2008;Mandal et al, 2019;Buckley et al, 2020). In addition, the BoB also receives a sizable freshwater influx from the rivers and undergoes near-surface ocean-atmosphere interactions, which alters the upper ocean processes (Parampil et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…In addition, the highly dynamic nature and the role of multiple factors affecting SSTs make it difficult to explore these relationships, if any. Some of the factors affecting SSTs are solar insolation, warm/cold water advection, and other marine processes, namely ocean currents, upwelling/downwelling phenomena, and eddies (Leeuwenburgh and Stammer, 2001;Shinoda, 2005;Krishna, 2008;Mandal et al, 2019;Buckley et al, 2020). In addition, the BoB also receives a sizable freshwater influx from the rivers and undergoes near-surface ocean-atmosphere interactions, which alters the upper ocean processes (Parampil et al, 2010).…”
Section: Introductionmentioning
confidence: 99%
“…The barotropic and baroclinic instability induced by the mean flow have been demonstrated to play an important role in the generation and evolution of eddies in extensive studies (e.g., Zu et al, 2013;Donohue et al, 2016;Li et al, 2016;Qian et al, 2018;Zhao et al, 2018;Mandal et al, 2019;Tedesco et al, 2019;Yang et al, 2020). Yang et al (2020) examined the instability and multiscale interactions underlying the LC eddy shedding based on the ensembles of flow fields output from a numerical model.…”
Section: Methodsmentioning
confidence: 99%
“…Of course, care should be taken in interpreting the details of the BT and BC conversions, because the global HYCOM (which assimilates observational data into the model) is not a free-run model that is required to conserve the total energy of the ocean system (e.g., Yang et al, 2020). However, we note that a similar approach has been taken to diagnose BT/BC conversion in several other studies using data assimilative models (e.g., Qian et al, 2018;Mandal et al, 2019). Energy transfer attributed to ocean dynamics can be separated from that introduced through data FIGURE 11 | Vertical distributions of (A) EKE (unit: m 2 /s 2 ), (B) EPE (unit: m 2 /s 2 ), (C) BT (unit: m 2 /s 3 ), and (D) BC (unit: m 2 /s 3 ) averaged horizontally over the effective eddy regions during phases 1-14 (April 9 to July 15, 2017).…”
Section: Mechanisms Behind the Growth And Evolution Of The Tortugas Eddymentioning
confidence: 98%
“…Coastal HFRs overcome all the above limitations, enabling the detection and tracking of the time history of surface eddies down to sub-mesoscale at the cost of a reduced spatial extent. Mandal et al (2019) provide quite an extensive list of recent literature reporting sub-mesoscale features observed by HFRs, with examples of observations in various coastal areas from the Atlantic to the Pacific and Indian oceans (Shay et al, 1995(Shay et al, , 2000Kirincich, 2016b;Archer et al, 2017;Lai et al, 2017;Arunraj et al, 2018). It is worth noticing that such features may have a strong vertical signature that HFR data fail to account for and therefore need to be complemented by further information spanning from direct measurements of the horizontal and vertical velocity profile to indications indirectly derived from, e.g., satellite turbidity measurements (see discussion in Uttieri et al, 2011).…”
Section: Eddy Trackingmentioning
confidence: 99%