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Artykuły w czasopismach na temat "Downwelling"
Kenyon, Kern E. "Downwelling by Surface Gravity Waves?" Natural Science 09, nr 05 (2017): 143–44. http://dx.doi.org/10.4236/ns.2017.95015.
Pełny tekst źródłaBlue, Charles. "Mantle downwelling causes continental depressions". Eos, Transactions American Geophysical Union 74, nr 9 (2.03.1993): 98. http://dx.doi.org/10.1029/93eo00359.
Pełny tekst źródłaCenedese, Claudia. "Downwelling in Basins Subject to Buoyancy Loss". Journal of Physical Oceanography 42, nr 11 (1.11.2012): 1817–33. http://dx.doi.org/10.1175/jpo-d-11-0114.1.
Pełny tekst źródłaFan, Wei, Dongdong Pan, Canbo Xiao, Tiancheng Lin, Yiwen Pan i Ying Chen. "Experimental Study on the Performance of an Innovative Tide-Induced Device for Artificial Downwelling". Sustainability 11, nr 19 (25.09.2019): 5268. http://dx.doi.org/10.3390/su11195268.
Pełny tekst źródłaBrüggemann, Nils, i Caroline A. Katsman. "Dynamics of Downwelling in an Eddying Marginal Sea: Contrasting the Eulerian and the Isopycnal Perspective". Journal of Physical Oceanography 49, nr 11 (listopad 2019): 3017–35. http://dx.doi.org/10.1175/jpo-d-19-0090.1.
Pełny tekst źródłaSpall, Michael A. "Buoyancy-Forced Downwelling in Boundary Currents". Journal of Physical Oceanography 38, nr 12 (1.12.2008): 2704–21. http://dx.doi.org/10.1175/2008jpo3993.1.
Pełny tekst źródłaMeneghello, Gianluca, John Marshall, Mary-Louise Timmermans i Jeffery Scott. "Observations of Seasonal Upwelling and Downwelling in the Beaufort Sea Mediated by Sea Ice". Journal of Physical Oceanography 48, nr 4 (kwiecień 2018): 795–805. http://dx.doi.org/10.1175/jpo-d-17-0188.1.
Pełny tekst źródłaFan, Wei, Weicheng Bao, Yong Cai, Canbo Xiao, Zhujun Zhang, Yiwen Pan, Ying Chen i Shuo Liu. "Experimental Study on the Effects of a Vertical Jet Impinging on Soft Bottom Sediments". Sustainability 12, nr 9 (6.05.2020): 3775. http://dx.doi.org/10.3390/su12093775.
Pełny tekst źródłaLiu, Shuo, Lige Zhao, Canbo Xiao, Wei Fan, Yong Cai, Yiwen Pan i Ying Chen. "Review of Artificial Downwelling for Mitigating Hypoxia in Coastal Waters". Water 12, nr 10 (13.10.2020): 2846. http://dx.doi.org/10.3390/w12102846.
Pełny tekst źródłaSpurgin, J. M., i S. E. Allen. "Flow dynamics around downwelling submarine canyons". Ocean Science 10, nr 5 (14.10.2014): 799–819. http://dx.doi.org/10.5194/os-10-799-2014.
Pełny tekst źródłaRozprawy doktorskie na temat "Downwelling"
Spurgin, Jessica Michelle. "Flow dynamics around downwelling submarine canyons". Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/46533.
Pełny tekst źródłaBhandari, 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.
Pełny tekst źródłaMehta, 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.
Pełny tekst źródłaWang, Haixing. "Impact Of Canyon Upwelling And Downwelling In The Mid-Atlantic Bight". W&M ScholarWorks, 2021. https://scholarworks.wm.edu/etd/1627407406.
Pełny tekst źródłaRodríguez, 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.
Pełny tekst źródłaCirculation 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 downwelling events, one of them with Lérez river ow increase. Also, was analyzed temporal series of uxes and ushing times through the external mouths and the correlations between these series and the forcing parameters (winds and average of the rivers ow). An EOF's study was applied to the subinertial normal velocities at the sections. Upwelling events are characterized by a reinforcement of the positive estuarine circulation, consistent with surface layer out ows and deep layer in ows at the main channel of the Ría, and in ows/out ows at the north/south mouths. Downwelling events have an opposite behaviour to the event described before. There are evidences of the vertical mixing through clockwise circulations at the outer part of the Ría, associated with the ocean waters subduction that enter into the Ría through the surface layer. As a consequence, a blocking can be generated at the middle part of the Ría, which has been associated by other authors with the "red tides". Fluxes for downwelling events are higher than for upwelling events. Flushing times are around 2 days for downwelling and around 4 days for upwelling events. The EOF's study con rms the circulation described for upwelling and downwelling events, in this work. The forecast of the physical conditions at Ría de Pontevedra are important for the understanding of the processes behind the production of HABs.
Diversos estudos tem sido realizados sobre os padrões de circulação em algumas das Rías Baixas, mas este não é o caso da Ría de Pontevedra. Ao longo desta tese tentaremos completar os conhecimentos sobre esta Ría. Uma con guração do sistema ROMS-AGRIF foi utilizada neste estudo, sendo esta validada com base na comparação com dados de temperatura e salinidade medidos semanalmente pelo INTECMAR. A analise realizada baseia-se no estudo de três episódios representativos da circulação: um de a oramento e dois de afundamento, um destes com caudal do río Lérez signi cativo. Foram ainda analisadas séries temporais de uxos e de tempos de renovação através de diversas secções. Foi analisada a correlação entre estas séries e os parâmetros forçadores (ventos e caudais dos rios). Foi realizado um estudo utilizando técnicas de funções empíricas ortogonais aplicado ao campo de velocidades normal às secções. Os eventos de a oramento são caracterizados por um reforço da circulação positiva na Ría, consistente com os uxos de saída pela camada superior e uxos de entrada pela camada inferior do canal principal da Ría, e com uxos de entrada pela boca norte e os uxos de saída pela boca sul. Nos eventos de afundamento o comportamento é oposto ao anterior. São discutidas evidências de recirculação vertical em forma de células no sentido dos ponteiros do relógio na zona externa da Ría, associado à subdução de águas oceânicas que entram na Ría pela camada superior. Este fenómeno parece criar uma zona de bloqueio no meio do eixo da Ría, que pode ser um mecanismo responsável pelo desenvolvimento das denominadas marés vermelhas. Os uxos para o evento de afundamento são superiores aos dos eventos de a oramento. O tempo de renovação é próximo dos 2 dias para o afundamento e dos 4 dias para o a oramento. O estudo por funções empíricas ortogonais con rma a circulação descrita durante os episódios de a oramento e afundamento discutidos neste trabalho. A previsão das condições físicas na Ría de Pontevedra é importante para a compreensão dos processos associados ao desenvolvimento de marés vermelhas.
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.
Pełny tekst źródłaNeal, David A. "Maximum Likelihood Temperature/Emissivity Separation of Hyperspectral Images with Gaussian Distributed Downwelling Radiance". DigitalCommons@USU, 2017. https://digitalcommons.usu.edu/etd/5873.
Pełny tekst źródłaViúdez, 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.
Pełny tekst źródłaLa radiació infrarroja a l’atmosfera és una component important del balanç energètic del planeta; en estar fortament relacionada amb l’efecte hivernacle influeix de manera remarcable en el clima. En aquest estudi s’avalua la bondat de les estimacions de la irradiància infrarroja incident en superfície (DLR) fetes amb un model unidimensional de transferència radiativa, el Santa Barbara DISORT Atmospheric Radiative Transfer (SBDART), per a condicions de cel serè o bé completament ennuvolat. Els càlculs realitzats amb aquest model han estat comparats amb mesures de pirgeòmetre realitzades en tres emplaçaments a Europa: Girona (NE de la Península Ibèrica), Payerne (a l’est de Suïssa), i Heselbach (a la Selva Negra, Alemanya). Els estudis de sensibilitat fets amb el model de transferència radiativa han mostrat l’especial importància que tenen els perfils atmosfèrics de temperatura i contingut d’aigua en absència de núvols; per cels completament ennuvolats l’estudi de sensibilitat mostra que, a banda dels perfils atmosfèrics esmentats, l’altura de la base dels núvols és molt rellevant. S’ha estimat la DLR per indrets on no es disposava de radiosondatges, substituint-los bé per un radiosondatge proper, o bé per perfils interpolats espacialment en l’anàlisi del model de predicció meteorològica de l’European Centre of Medium-Range Weather Forecast (ECMWF). Els càlculs han estat comparats amb mesures per tots els llocs. Per condicions de cel serè, i quan es disposa de radiosondatge, els càlculs mostren una diferència amb les mesures de -2.7 ± 3.4 Wm-2 (Payerne). Quan no es disposa d’aquests perfils, la diferència entre les modelitzacions i les mesures és de 0.3 ± 9.4 Wm-2 (Girona). Per condicions de cel cobert, quan es disposa del radiosondatge i les propietats dels núvols (derivades a partir d’un algoritme que empra mesures espectrals en infraroig i en la banda de microones en superfície, Selva Negra), els càlculs mostren una diferència amb les mesures de -0.28 ± 2.52 Wm-2. Quan es fan servir els perfils del ECMWF i es fixa el valor de la columna d’aigua líquida i el radi efectiu de les gotes d’aigua (Girona) els càlculs mostren una diferència amb les mesures de 4.0 ± 2.5 Wm-2. També s’ha confirmat per totes les condicions estudiades que les estimacions amb el model de transferència radiativa són notablement millors que les obtingudes amb parametritzacions senzilles de l’emissivitat atmosfèrica.
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.
Pełny tekst źródłaAbstract
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.
Pełny tekst źródłaKsiążki na temat "Downwelling"
Chance, Kelly, i Randall V. Martin. Modeling Radiative Transfer. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199662104.003.0009.
Pełny tekst źródłaRuxton, Graeme D., William L. Allen, Thomas N. Sherratt i Michael P. Speed. Countershading. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780199688678.003.0004.
Pełny tekst źródłaCzęści książek na temat "Downwelling"
Mohan, Ram K., Andrew D. Short, Gillian Cambers, M. MacLeod, J. A. G. Cooper, David Hopley, Vincent May i in. "Coastal Upwelling and Downwelling". W Encyclopedia of Coastal Science, 306–8. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_88.
Pełny tekst źródłaBarua, Dilip K. "Coastal Upwelling and Downwelling". W 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.
Pełny tekst źródłaBarua, Dilip K. "Coastal Upwelling and Downwelling". W Encyclopedia of Earth Sciences Series, 600–604. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93806-6_88.
Pełny tekst źródłaStathopoulos, V., i C. Matsoukas. "Long-Term Memory and Multifractality of Downwelling Longwave Flux at Stations Worldwide". W Perspectives on Atmospheric Sciences, 1193–98. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-35095-0_172.
Pełny tekst źródłaFrank, Tamara M., i 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". W Zooplankton: sensory ecology and physiology, 185–93. London: Routledge, 2021. http://dx.doi.org/10.1201/9780203733615-13.
Pełny tekst źródła"downwelling". W Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik, 409. Berlin, Heidelberg: Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_43318.
Pełny tekst źródłaCarder, Kendall L., i David K. Costello. "Optical Effects of Large Particles". W Ocean Optics. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195068436.003.0017.
Pełny tekst źródłaWalker, James C. G. "How to Solve a Nonlinear System". W Numerical Adventures with Geochemical Cycles. Oxford University Press, 1991. http://dx.doi.org/10.1093/oso/9780195045208.003.0006.
Pełny tekst źródłaKING, S. "Mantle Downwellings and the Fate of Subducting Slabs: Constraints from Seismology, Geoid Topography, Geochemistry, and Petrology". W Treatise on Geophysics, 325–70. Elsevier, 2007. http://dx.doi.org/10.1016/b978-044452748-6/00122-x.
Pełny tekst źródłaKing, S. D. "Mantle Downwellings and the Fate of Subducting Slabs: Constraints from Seismology, Geoid Topography, Geochemistry, and Petrology". W Treatise on Geophysics, 325–70. Elsevier, 2007. http://dx.doi.org/10.1016/b978-044452748-6.00122-x.
Pełny tekst źródłaStreszczenia konferencji na temat "Downwelling"
Pieper, M., D. Manolakis, E. Truslow, T. Cooley, M. Brueggeman, A. Weisner i J. Jacobson. "In-scene LWIR downwelling radiance estimation". W SPIE Optical Engineering + Applications, redaktorzy John F. Silny i Emmett J. Ientilucci. SPIE, 2016. http://dx.doi.org/10.1117/12.2239138.
Pełny tekst źródłaSlegel, David A., i T. D. Dickey. "Characterization Of Downwelling Spectral Irradiance Fluctuations". W 1988 Technical Symposium on Optics, Electro-Optics, and Sensors, redaktor Marvin A. Blizard. SPIE, 1988. http://dx.doi.org/10.1117/12.945710.
Pełny tekst źródłaLinnemann, K., P. Gege, S. Rößler, T. Schneider i A. Melzer. "CDOM retrieval using measurements of downwelling irradiance". W SPIE Remote Sensing, redaktorzy Charles R. Bostater, Stelios P. Mertikas i Xavier Neyt. SPIE, 2013. http://dx.doi.org/10.1117/12.2031250.
Pełny tekst źródłaGoforth, Mark A., George W. Gilchrist i Joseph D. Sirianni. "Cloud effects on thermal downwelling sky radiance". W AeroSense 2002, redaktorzy Xavier P. Maldague i Andres E. Rozlosnik. SPIE, 2002. http://dx.doi.org/10.1117/12.459570.
Pełny tekst źródłaGroetsch, Philipp, i Peter Gege. "Determination of sensor depth from downwelling irradiance measurements". W IGARSS 2012 - 2012 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2012. http://dx.doi.org/10.1109/igarss.2012.6350835.
Pełny tekst źródłaTessendorf, Jerry A. "Downwelling irradiance fluctuations in the small-angle approximation". W Orlando '90, 16-20 April, redaktor Richard W. Spinrad. SPIE, 1990. http://dx.doi.org/10.1117/12.34724.
Pełny tekst źródłaEstep, Leland. "Spectral eigenanalysis of up- and downwelling k profiles". W San Diego '92, redaktor Gary D. Gilbert. SPIE, 1992. http://dx.doi.org/10.1117/12.140657.
Pełny tekst źródłaWurst, Nathan P., Joseph Meola i David L. Perry. "Measurement and modeling of longwave infrared directional downwelling spectral radiance". W SPIE Optical Engineering + Applications, redaktorzy Thomas S. Pagano i John F. Silny. SPIE, 2015. http://dx.doi.org/10.1117/12.2186557.
Pełny tekst źródłaMlynczak, Martin G., Richard P. Cageao, Harri Latvakoski, David P. Kratz, Jeffrey Mast i David G. Johnson. "Observations Of Downwelling Far-Infrared Radiance At Earth’s Surface with FIRST". W Hyperspectral Imaging and Sounding of the Environment. Washington, D.C.: OSA, 2015. http://dx.doi.org/10.1364/hise.2015.ht4b.4.
Pełny tekst źródłaTiwari, Surya Prakash, Y. V. B. Sarma i Burton H. Jones. "Evaluation of downwelling diffuse attenuation coefficient algorithms in the Red Sea". W SPIE Asia-Pacific Remote Sensing, redaktorzy Robert J. Frouin, Satheesh C. Shenoi i K. H. Rao. SPIE, 2016. http://dx.doi.org/10.1117/12.2222823.
Pełny tekst źródłaRaporty organizacyjne na temat "Downwelling"
Voss, Kenneth J. Polarized Downwelling Radiance Distribution Camera System. Fort Belvoir, VA: Defense Technical Information Center, styczeń 2008. http://dx.doi.org/10.21236/ada516872.
Pełny tekst źródłaFinkel, R. Evidence for Stratospheric Downwelling Associated with High-Elevation Topography. Office of Scientific and Technical Information (OSTI), styczeń 2009. http://dx.doi.org/10.2172/947744.
Pełny tekst źródłaLong, CN, P. Gotseff i EG Dutton. Investigation of the Downwelling LW Differences Between the Niamey AMF Main and Supplementary Sites. Office of Scientific and Technical Information (OSTI), kwiecień 2008. http://dx.doi.org/10.2172/948029.
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