Relevant bibliographies by topics / Downwelling

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Downwelling'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Downwelling"

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Kenyon, Kern E. "Downwelling by Surface Gravity Waves?" Natural Science 09, no. 05 (2017): 143–44. http://dx.doi.org/10.4236/ns.2017.95015.

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Blue, Charles. "Mantle downwelling causes continental depressions." Eos, Transactions American Geophysical Union 74, no. 9 (March 2, 1993): 98. http://dx.doi.org/10.1029/93eo00359.

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Cenedese, Claudia. "Downwelling in Basins Subject to Buoyancy Loss." Journal of Physical Oceanography 42, no. 11 (November 1, 2012): 1817–33. http://dx.doi.org/10.1175/jpo-d-11-0114.1.

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Abstract Recent observational, theoretical, and modeling studies all suggest that the upper part of the downwelling limb of the thermohaline circulation is concentrated in strong currents subject to buoyancy loss near lateral boundaries. This is fundamentally different from the traditional view that downwelling takes place in regions of deep convection. Even when resolving the buoyant boundary currents, coarse-resolution global circulation and climate models rely on parameterizations of poorly known turbulent mixing processes. In this study, the first direct measurements of downwelling occurri
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Fan, Wei, Dongdong Pan, Canbo Xiao, Tiancheng Lin, Yiwen Pan, and Ying Chen. "Experimental Study on the Performance of an Innovative Tide-Induced Device for Artificial Downwelling." Sustainability 11, no. 19 (September 25, 2019): 5268. http://dx.doi.org/10.3390/su11195268.

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Hypoxia has been increasingly observed in estuaries and coastal marine ecosystems around the world. In this paper, a tide-powered artificial downwelling device is proposed to potentially alleviate hypoxia in bottom waters. The downwelling device mainly consists of a vertical square tube, a 90° bend sitting on the top of the tube, two symmetrical-guide plates which installed alongside the vertical tube, a static mixer, and an artificial reef. Scale model experiments are performed with respect to different density difference heads, horizontal current velocities, and tube geometries. The results
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Brüggemann, Nils, and Caroline A. Katsman. "Dynamics of Downwelling in an Eddying Marginal Sea: Contrasting the Eulerian and the Isopycnal Perspective." Journal of Physical Oceanography 49, no. 11 (November 2019): 3017–35. http://dx.doi.org/10.1175/jpo-d-19-0090.1.

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AbstractIn this study, we explore the downward branch of the Atlantic meridional overturning circulation (AMOC) from a perspective in depth space (Eulerian downwelling) as well as from a perspective in density space (diapycnal downwelling). Using an idealized model, we focus on the role of eddying marginal seas, where dense water is formed by deep convection due to an intense surface heat loss. We assess where diapycnal mass fluxes take place, investigate the pathways of dense water masses, and elucidate the role of eddies. We find that there are fundamental differences between the Eulerian an
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Spall, Michael A. "Buoyancy-Forced Downwelling in Boundary Currents." Journal of Physical Oceanography 38, no. 12 (December 1, 2008): 2704–21. http://dx.doi.org/10.1175/2008jpo3993.1.

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Abstract The issue of downwelling resulting from surface buoyancy loss in boundary currents is addressed using a high-resolution, nonhydrostatic numerical model. It is shown that the net downwelling is determined by the change in the mixed layer density along the boundary. For configurations in which the density on the boundary increases in the direction of Kelvin wave propagation, there is a net downwelling within the domain. For cases in which the density decreases in the direction of Kelvin wave propagation, cooling results in a net upwelling within the domain. Symmetric instability within
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Meneghello, Gianluca, John Marshall, Mary-Louise Timmermans, and Jeffery Scott. "Observations of Seasonal Upwelling and Downwelling in the Beaufort Sea Mediated by Sea Ice." Journal of Physical Oceanography 48, no. 4 (April 2018): 795–805. http://dx.doi.org/10.1175/jpo-d-17-0188.1.

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AbstractWe present observational estimates of Ekman pumping in the Beaufort Gyre region. Averaged over the Canada Basin, the results show a 2003–14 average of 2.3 m yr−1 downward with strong seasonal and interannual variability superimposed: monthly and yearly means range from 30 m yr−1 downward to 10 m yr−1 upward. A clear, seasonal cycle is evident with intense downwelling in autumn and upwelling during the winter months, despite the wind forcing being downwelling favorable year-round. Wintertime upwelling is associated with friction between the large-scale Beaufort Gyre ocean circulation an
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Fan, Wei, Weicheng Bao, Yong Cai, Canbo Xiao, Zhujun Zhang, Yiwen Pan, Ying Chen, and Shuo Liu. "Experimental Study on the Effects of a Vertical Jet Impinging on Soft Bottom Sediments." Sustainability 12, no. 9 (May 6, 2020): 3775. http://dx.doi.org/10.3390/su12093775.

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Artificial downwelling, which is an ecological engineering method, potentially alleviates bottom hypoxia by bringing oxygen-rich surface water down below the pycnocline. However, the downward flow is likely to disturb sediments (or induce sediment resuspension) when reaching the bottom and then have unwanted side effects on the local ecosystem. To evaluate this, our paper presents a theoretical model and experimental data for the sediment resuspension caused by artificial downwelling. The theoretical model considers the critical conditions for sediment resuspension and the scour volume with th
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Liu, Shuo, Lige Zhao, Canbo Xiao, Wei Fan, Yong Cai, Yiwen Pan, and Ying Chen. "Review of Artificial Downwelling for Mitigating Hypoxia in Coastal Waters." Water 12, no. 10 (October 13, 2020): 2846. http://dx.doi.org/10.3390/w12102846.

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Hypoxia is becoming a serious problem in coastal waters in many parts of the world. Artificial downwelling, which is one of the geoengineering-based adaptation options, was suggested as an effective means of mitigating hypoxia in coastal waters. Artificial downwelling powered by green energy, such as solar, wind, wave, or tidal energy, can develop a compensatory downward flow on a kilometer scale, which favors below-pycnocline ventilation and thus mitigates hypoxia in bottom water. In this paper, we review and assess the technical, numerical, and experimental aspects of artificial downwelling
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Spurgin, J. M., and S. E. Allen. "Flow dynamics around downwelling submarine canyons." Ocean Science 10, no. 5 (October 14, 2014): 799–819. http://dx.doi.org/10.5194/os-10-799-2014.

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Abstract. Flow dynamics around a downwelling submarine canyon were analysed with the Massachusetts Institute of Technology general circulation model. Blanes Canyon (northwestern Mediterranean) was used for topographic and initial forcing conditions. Fourteen scenarios were modelled with varying forcing conditions. Rossby and Burger numbers were used to determine the significance of Coriolis acceleration and stratification (respectively) and their impacts on flow dynamics. A new non-dimensional parameter (χ) was introduced to determine the significance of vertical variations in stratification.
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Dissertations / Theses on the topic "Downwelling"

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Spurgin, Jessica Michelle. "Flow dynamics around downwelling submarine canyons." Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/46533.

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Flow dynamics around a downwelling submarine canyon were analyzed with the Massachusetts Institute of Technology general circulation model. Blanes Canyon (Northwest Mediterranean) was used for topographic and initial forcing conditions. Fourteen scenarios were modelled with varying forcing conditions. Rossby number and Burger number were used to determine the significance of Coriolis acceleration and stratification (respectively) and their impacts on flow dynamics. A new non-dimensional parameter (χ) was introduced to determine the significance of vertical variations in stratification. Downwel
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Bhandari, Purushottam. "The Design of a Polarimeter and its Use for the Study of the Variation of Downwelling Polarized Radiance Distribution with Depth in the Ocean." Scholarly Repository, 2011. http://scholarlyrepository.miami.edu/oa_dissertations/605.

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The spectral polarized radiance distribution provides the most complete description of the light field that can be measured. However, this is a very difficult parameter to measure near the surface because of its large dynamic range, dependence on incoming sky conditions, and waves at the air-sea interface. The measurement of the Stokes vector of the downwelling polarized light field requires the combination of at least four images, all of which must be obtained simultaneously. To achieve this, a new polarimeter (which we call DPOL) has been designed, characterized, calibrated and deployed. T
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Mehta, Payal. "The microphysical properties of Saharan dust obtainable from downwelling infrared radiances." Thesis, Imperial College London, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.526395.

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Wang, Haixing. "Impact Of Canyon Upwelling And Downwelling In The Mid-Atlantic Bight." W&M ScholarWorks, 2021. https://scholarworks.wm.edu/etd/1627407406.

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Submarine canyons can impact regional oceanography and provide a conduit for shelf-slope exchanges via topographically induced processes such as canyon upwelling and downwelling. Between Virginia and New York in the Mid-Atlantic Bight (MAB), there are five major shelf-incising canyons (Norfolk, Washington, Baltimore, Wilmington, and Hudson canyons) and four sizable slope-confined canyons (Accomac, Spencer, Lindenkhol, and Toms canyons). Canyon upwelling and downwelling at these canyons have not been well studied. Consequently, the associated hydrographic variability and dynamics inside the can
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Rodríguez, Cruz Elisabet. "Circulation patterns of Ría de Pontevedra under upwelling and downwelling conditions." Master's thesis, Universidade de Aveiro, 2017. http://hdl.handle.net/10773/23481.

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Mestrado em Ciências do Mar e da Atmosfera<br>Circulation patterns inside some of the Rías Baixas have been widely studied, but this is not the case of the Ría de Pontevedra. Through this thesis, we try to enhance the knowledge about the circulation pattern of this Ría. A ROMS-AGRIF system con guration was used in this study. This con guration was validated through the comparison with weekly temperature and salinity data measured by INTECMAR. The analysis done in this work is based on the study of three representative events of the circulation patterns: one upwelling event and two downw
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Zhang, Zhenxi. "Modeling downwelling circulation over continental shelf in the northern South China Sea /." View abstract or full-text, 2009. http://library.ust.hk/cgi/db/thesis.pl?AMCE%202009%20ZHANG.

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Neal, David A. "Maximum Likelihood Temperature/Emissivity Separation of Hyperspectral Images with Gaussian Distributed Downwelling Radiance." DigitalCommons@USU, 2017. https://digitalcommons.usu.edu/etd/5873.

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Hyperspectral images are made up of energy measurements at different wavelengths of light. The case is considered where these measurements are dependent on temperature, the self-emitted energy (emissivity), and reflected energy (downwelling radiance) from the surroundings. The process where the downwelling radiance is fixed and the temperature and emissivity are estimated is referred to as temperature/emissivity separation. Due to the way these terms mix, for a given set of measurements, there exist many pairs of temperatures and emissivities that satisfy the model. This creates ambiguity in t
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Viúdez, i. Mora Antoni. "Atmospheric downwelling longwave radiation at the surface during cloudless and overcast conditions. Measurements and modeling." Doctoral thesis, Universitat de Girona, 2011. http://hdl.handle.net/10803/31841.

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Atmospheric downwelling longwave radiation is an important component of the terrestrial energy budget; since it is strongly related with the greenhouse effect, it remarkably affects the climate. In this study, I evaluate the estimation of the downwelling longwave irradiance at the terrestrial surface for cloudless and overcast conditions using a one-dimensional radiative transfer model (RTM), specifically the Santa Barbara DISORT Atmospheric Radiative Transfer (SBDART). The calculations performed by using this model were compared with pyrgeometer measurements at three different European places
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Batifoulier, François. "Hydrodynamique du plateau continental aquitain et influence sur les épisodes à Dinophysis dans le Bassin d’Arcachon." Thesis, Bordeaux 1, 2011. http://www.theses.fr/2011BOR14441/document.

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Des épisodes à Dinophysis affectent périodiquement l'exploitation des fruits de mer dans le Bassin d'Arcachon. Le réseau de surveillance interne au Bassin d'Arcachon montre que Dinophysis est advecté de l'océan ouvert. Le but de cette étude est de déterminer l'origine de Dinophysis. Des campagnes en mer sur le plateau continental Aquitain ont permis d'identifier une zone propice au développement de Dinophysis au large de Capbreton. Les épisodes à Dinophysis dans le bassin d'Arcachon se produisent suite à des vents d'Ouest qui induisent des courants vers le Sud d'après la littérature. L'étude d
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Logvinov, Evgeny. "Two responses of a uniformly stratified flow over a sloping bottom to a spatially varying downwelling favorable wind." Thesis, Online version of original thesis, 2008. http://hdl.handle.net/1912/2500.

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Books on the topic "Downwelling"

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Chance, Kelly, and Randall V. Martin. Modeling Radiative Transfer. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199662104.003.0009.

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Basic concepts and definitions of radiative transfer modeling are introduced. The applicability of single scattering to aerosol retrievals is demonstrated. A two-stream formulation of radiative transfer is introduced. The two streams, upwelling and downwelling radiation, are selected to angularly represent average atmospheric properties: Relatively simple, two-stream calculations form the basis for much practical calculation, particularly of hemispherical fluxes in stratified atmospheres. Following this development, the most usual method for replacing the general integrodifferential equations
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Ruxton, Graeme D., William L. Allen, Thomas N. Sherratt, and Michael P. Speed. Countershading. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199688678.003.0004.

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Countershading is a coloration pattern where the exterior surfaces most exposed to light, typically dorsal surfaces, are more darkly coloured than those oriented away from light, typically ventral surfaces. Countershading is widely discussed as a camouflage defence, although other functions—such as thermoregulation, abrasion resistance, and protection from ultraviolet light—may also select for countershading. In terms of camouflage, countershading is thought to work by up to six distinct mechanisms. We discuss several key examples of countershading and counterillumination that give insight int
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Book chapters on the topic "Downwelling"

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Mohan, Ram K., Andrew D. Short, Gillian Cambers, M. MacLeod, J. A. G. Cooper, David Hopley, Vincent May, et al. "Coastal Upwelling and Downwelling." In Encyclopedia of Coastal Science, 306–8. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_88.

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Barua, Dilip K. "Coastal Upwelling and Downwelling." In Encyclopedia of Earth Sciences Series, 1–5. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-48657-4_88-2.

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Barua, Dilip K. "Coastal Upwelling and Downwelling." In Encyclopedia of Earth Sciences Series, 600–604. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_88.

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Stathopoulos, V., and C. Matsoukas. "Long-Term Memory and Multifractality of Downwelling Longwave Flux at Stations Worldwide." In Perspectives on Atmospheric Sciences, 1193–98. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-35095-0_172.

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Frank, Tamara M., and Edith A. Widder. "UV Light in the Deep-Sea: In Situ Measurements of Downwelling Irradiance in Relation to the Visual Threshold Sensitivity of UV-Sensitive Crustaceans." In Zooplankton: sensory ecology and physiology, 185–93. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203733615-13.

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"downwelling." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 409. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_43318.

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Carder, Kendall L., and David K. Costello. "Optical Effects of Large Particles." In Ocean Optics. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195068436.003.0017.

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Two important problems facing the ocean optics research community in the coming decade concern optical model closure and inversion (see Chapter 3). We obtain model closure if we can describe the measured light environment by combining elementary measurements of the optical properties of the medium with radiative transfer theory. If we can accurately deduce the concentration of various constituents from a combination of measures of the submarine light field and inverse model calculations, we term this process model inversion. The most elementary measurements of the optical properties of the sea are those that are independent of the geometry of the light field, the inherent optical properties (Preisendorfer, 1961). Optical properties that are dependent on the geometry of the light field are termed apparent optical properties (AOP). Models of the submarine light field typically relate apparent optical properties to inherent optical properties (see Chapter 2). Examples include the relationship between the AOP irradiance reflectance R and a combination of inherent optical properties (backscattering coefficient bb and absorption coefficient a), and the relationship between the AOP downwelling diffuse attenuation coefficient kd and a combination of the absorption coefficient, backscattering coefficient, and downwelling average cosine μd (e.g., Gordon et al., 1975; Morel and Prieur, 1977; Smith and Baker, 1981; Morel, 1988; Kirk, 1984a). Under some circumstances these relationships work well enough that the absorption coefficient can be derived indirectly. This is important since measurement of the absorption coefficient by direct means has been difficult. Derived values for the absorption coefficient by model inversion methods are not easily verified by independent measurements, however, because of the difficulty of measuring the absorption coefficient. Model closure and model inversion both become more tenuous when the following phenomena are present: 1. Transpectral or inelastic scattering such as fluorescence (e.g., Gordon, 1979; Carder and Steward, 1985; Mitchell and Kiefer, 1988a; Spitzer and Dirks, 1985; Hawes and Carder, 1990) or water Raman scattering (Marshall and Smith, 1990; Stavn, 1990; Stavn and Weidemann, 1988a,b; Peacock et al, 1990; Chapter 12 this volume). 2. Particles that are large relative to the measurement volume for inherent optical property meters such as beam transmissometers, light-scattering photometers, fluorometers, and absorption meters.
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Walker, James C. G. "How to Solve a Nonlinear System." In Numerical Adventures with Geochemical Cycles. Oxford University Press, 1991. http://dx.doi.org/10.1093/oso/9780195045208.003.0006.

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In a linear system the expressions, yp, for rates of change are linear functions of the dependent variables, y. More complicated functions of y do not appear, not even products of the dependent variables like y1 * y2. But most theoretical problems in Earth system science involve nonlinearities. For example, the rate at which a chemical reaction consumes species 1 may be proportional to the product of the concentrations of species 1 and the species 2 with which it is reacting, y1 * y2. In this chapter I shall describe and solve a simple nonlinear system involving the reaction between dissolved oxygen and organic carbon in the deep sea. I shall show how the nonlinear system can be represented by a linear system, provided that changes in the dependent variables are made in sufficiently small increments. Such increments are kept small by stepping forward in time with small steps. The time step can be adjusted automatically during the calculation so as to keep the increments small enough but no smaller than necessary. Steps that are too large cause errors or even instability, and steps that are too small waste time. The representation of a nonlinear system by its linear equivalent (for small increments) calls on algebraic manipulations that can be tedious and a prolific source of mistakes in complicated systems. This algebra can be avoided, however, by letting the computer perform the equivalent manipulations numerically. I shall demonstrate how to do this, finishing the chapter with a program that can solve coupled nonlinear systems directly from the equations for the rates of change of the dependent variables, automatically adjusting the time step to small values when the rates of change are large and to large values when the rates of change are small. Figure 4-1 shows a simple model of the processes that control the oxygen balance of the deep sea. Dissolved oxygen in surface seawater equilibrates with the atmosphere. Downwelling currents carry dissolved oxygen into the deep sea, where most of it reacts (metabolically) with organic matter carried into the deep sea in the form of settling particles of biological origin.
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KING, S. "Mantle Downwellings and the Fate of Subducting Slabs: Constraints from Seismology, Geoid Topography, Geochemistry, and Petrology." In Treatise on Geophysics, 325–70. Elsevier, 2007. http://dx.doi.org/10.1016/b978-044452748-6/00122-x.

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King, S. D. "Mantle Downwellings and the Fate of Subducting Slabs: Constraints from Seismology, Geoid Topography, Geochemistry, and Petrology." In Treatise on Geophysics, 325–70. Elsevier, 2007. http://dx.doi.org/10.1016/b978-044452748-6.00122-x.

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Conference papers on the topic "Downwelling"

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Pieper, M., D. Manolakis, E. Truslow, T. Cooley, M. Brueggeman, A. Weisner, and J. Jacobson. "In-scene LWIR downwelling radiance estimation." In SPIE Optical Engineering + Applications, edited by John F. Silny and Emmett J. Ientilucci. SPIE, 2016. http://dx.doi.org/10.1117/12.2239138.

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Slegel, David A., and T. D. Dickey. "Characterization Of Downwelling Spectral Irradiance Fluctuations." In 1988 Technical Symposium on Optics, Electro-Optics, and Sensors, edited by Marvin A. Blizard. SPIE, 1988. http://dx.doi.org/10.1117/12.945710.

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Linnemann, K., P. Gege, S. Rößler, T. Schneider, and A. Melzer. "CDOM retrieval using measurements of downwelling irradiance." In SPIE Remote Sensing, edited by Charles R. Bostater, Stelios P. Mertikas, and Xavier Neyt. SPIE, 2013. http://dx.doi.org/10.1117/12.2031250.

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Goforth, Mark A., George W. Gilchrist, and Joseph D. Sirianni. "Cloud effects on thermal downwelling sky radiance." In AeroSense 2002, edited by Xavier P. Maldague and Andres E. Rozlosnik. SPIE, 2002. http://dx.doi.org/10.1117/12.459570.

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Groetsch, Philipp, and Peter Gege. "Determination of sensor depth from downwelling irradiance measurements." In IGARSS 2012 - 2012 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2012. http://dx.doi.org/10.1109/igarss.2012.6350835.

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Tessendorf, Jerry A. "Downwelling irradiance fluctuations in the small-angle approximation." In Orlando '90, 16-20 April, edited by Richard W. Spinrad. SPIE, 1990. http://dx.doi.org/10.1117/12.34724.

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Estep, Leland. "Spectral eigenanalysis of up- and downwelling k profiles." In San Diego '92, edited by Gary D. Gilbert. SPIE, 1992. http://dx.doi.org/10.1117/12.140657.

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Wurst, Nathan P., Joseph Meola, and David L. Perry. "Measurement and modeling of longwave infrared directional downwelling spectral radiance." In SPIE Optical Engineering + Applications, edited by Thomas S. Pagano and John F. Silny. SPIE, 2015. http://dx.doi.org/10.1117/12.2186557.

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Mlynczak, Martin G., Richard P. Cageao, Harri Latvakoski, David P. Kratz, Jeffrey Mast, and David G. Johnson. "Observations Of Downwelling Far-Infrared Radiance At Earth’s Surface with FIRST." In Hyperspectral Imaging and Sounding of the Environment. Washington, D.C.: OSA, 2015. http://dx.doi.org/10.1364/hise.2015.ht4b.4.

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Tiwari, Surya Prakash, Y. V. B. Sarma, and Burton H. Jones. "Evaluation of downwelling diffuse attenuation coefficient algorithms in the Red Sea." In SPIE Asia-Pacific Remote Sensing, edited by Robert J. Frouin, Satheesh C. Shenoi, and K. H. Rao. SPIE, 2016. http://dx.doi.org/10.1117/12.2222823.

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Reports on the topic "Downwelling"

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Voss, Kenneth J. Polarized Downwelling Radiance Distribution Camera System. Fort Belvoir, VA: Defense Technical Information Center, January 2008. http://dx.doi.org/10.21236/ada516872.

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Finkel, R. Evidence for Stratospheric Downwelling Associated with High-Elevation Topography. Office of Scientific and Technical Information (OSTI), January 2009. http://dx.doi.org/10.2172/947744.

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Long, CN, P. Gotseff, and EG Dutton. Investigation of the Downwelling LW Differences Between the Niamey AMF Main and Supplementary Sites. Office of Scientific and Technical Information (OSTI), April 2008. http://dx.doi.org/10.2172/948029.

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