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Relevant bibliographies by topics / Diagnosing stirring in the Bay of Bengal

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Academic literature on the topic 'Diagnosing stirring in the Bay of Bengal'

Author: Grafiati

Published: 6 September 2023

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Journal articles on the topic "Diagnosing stirring in the Bay of Bengal"

1

Paul, Nihar, and Jai Sukhatme. "Seasonality of surface stirring by geostrophic flows in the Bay of Bengal." Deep Sea Research Part II: Topical Studies in Oceanography 172 (February 2020): 104684. http://dx.doi.org/10.1016/j.dsr2.2019.104684.

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2

Jaeger, G. Spiro, J. A. MacKinnon, A. J. Lucas, et al. "How Spice is Stirred in the Bay of Bengal." Journal of Physical Oceanography 50, no. 9 (2020): 2669–88. http://dx.doi.org/10.1175/jpo-d-19-0077.1.

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AbstractThe scale-dependent variance of tracer properties in the ocean bears the imprint of the oceanic eddy field. Anomalies in spice (which combines anomalies in temperature T and salinity S on isopycnal surfaces) act as passive tracers beneath the surface mixed layer (ML). We present an analysis of spice distributions along isopycnals in the upper 200 m of the ocean, calculated with over 9000 vertical profiles of T and S measured along ~4800 km of ship tracks in the Bay of Bengal. The data are from three separate research cruises—in the winter monsoon season of 2013 and in the late and earl

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3

Bellon, Gilles, Adam H. Sobel, and Jerome Vialard. "Ocean–Atmosphere Coupling in the Monsoon Intraseasonal Oscillation: A Simple Model Study." Journal of Climate 21, no. 20 (2008): 5254–70. http://dx.doi.org/10.1175/2008jcli2305.1.

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Abstract A simple coupled model is used in a zonally symmetric aquaplanet configuration to investigate the effect of ocean–atmosphere coupling on the Asian monsoon intraseasonal oscillation. The model consists of a linear atmospheric model of intermediate complexity based on quasi-equilibrium theory coupled to a simple, linear model of the upper ocean. This model has one unstable eigenmode with a period in the 30–60-day range and a structure similar to the observed northward-propagating intraseasonal oscillation in the Bay of Bengal/west Pacific sector. The ocean–atmosphere coupling is shown t

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4

Pandey, Lokesh Kumar, Suneet Dwivedi, and Alok Kumar Mishra. "Diagnosing the upper ocean variability in the Northern Bay of Bengal during the super cyclone Phailin using a high-resolution regional ocean model." Theoretical and Applied Climatology, November 11, 2022. http://dx.doi.org/10.1007/s00704-022-04275-2.

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Dissertations / Theses on the topic "Diagnosing stirring in the Bay of Bengal"

1

Paul, Nihar. "Stirring and mixing driven by mesoscale eddies in the stratified Bay of Bengal." Thesis, 2022. https://etd.iisc.ac.in/handle/2005/5855.

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The stirring of passive tracers driven by altimetry-derived daily surface geostrophic currents is studied on subseasonal timescales in the Bay of Bengal. Advection of latitudinal and longitudinal bands highlights the chaotic nature of stirring in the Bay via repeated straining and filamentation of the tracer field. An immediate finding is that stirring is local, i.e., of the scale of the eddies, and does not span the entire basin. Further, stirring rates are enhanced along the coast of the Bay and are relatively higher in the pre-and post-monsoonal seasons. The spatially non-uniform stirring a

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