Готові списки джерел за темами / Ocean-atmosphere interaction

Добірка наукової літератури з теми "Ocean-atmosphere interaction"

Автор: Grafiati
Опубліковано: 4 червня 2021
Оновлено: 31 липня 2024

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Статті в журналах з теми "Ocean-atmosphere interaction"

1

Buat-Ménard(Bordeaux), P. "Atmosphere-ocean interaction." Journal of Marine Systems 8, no. 1-2 (May 1996): 131–32. http://dx.doi.org/10.1016/s0924-7963(96)90010-x.

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2

Lifland, Jonathan. "Earth's Climate:The Ocean-Atmosphere Interaction." Eos, Transactions American Geophysical Union 85, no. 46 (2004): 486. http://dx.doi.org/10.1029/2004eo460009.

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3

Derand, Pierre. "Ocean-atmosphere interaction and climate modelling." Atmospheric Research 39, no. 4 (December 1995): 355–56. http://dx.doi.org/10.1016/0169-8095(95)90012-8.

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4

Hughes, Tertia M. C. "Ocean-atmosphere interaction and climate modelling." Dynamics of Atmospheres and Oceans 25, no. 4 (May 1997): 273–75. http://dx.doi.org/10.1016/0377-0265(95)00464-5.

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5

Tett, Simon. "Ocean-Atmosphere interaction and climate modelling." Journal of Experimental Marine Biology and Ecology 194, no. 2 (December 1995): 287–89. http://dx.doi.org/10.1016/0022-0981(95)90099-3.

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6

Moulin, A., and A. Wirth. "A Drag-Induced Barotropic Instability in Air–Sea Interaction." Journal of Physical Oceanography 44, no. 2 (February 1, 2014): 733–41. http://dx.doi.org/10.1175/jpo-d-13-097.1.

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Abstract A new mechanism that induces barotropic instability in the ocean is discussed. It is due to the air–sea interaction with a quadratic drag law and horizontal viscous dissipation in the atmosphere. The authors show that the instability spreads to the atmosphere. The preferred spatial scale of the instability is that of the oceanic baroclinic Rossby radius of deformation. It can only be represented in numerical models, when the dynamics at this scale is resolved in the atmosphere and ocean. The dynamics are studied using two superposed shallow water layers: one for the ocean and one for the atmosphere. The interaction is due to the shear between the two layers. The shear applied to the ocean is calculated using the velocity difference between the ocean and the atmosphere and the quadratic drag law. In one-way interaction, the shear applied to the atmosphere neglects the ocean dynamics; it is calculated using the atmospheric wind only. In two-way interaction, it is opposite to the shear applied to the ocean. In one-way interaction, the atmospheric shear leads to a barotropic instability in the ocean. The instability in the ocean is amplified, in amplitude and scale, in two-way interaction and also triggers an instability in the atmosphere.
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7

Chelton, Dudley, and Shang-Ping Xie. "Coupled Ocean-Atmosphere Interaction at Oceanic Mesoscales." Oceanography 23, no. 4 (December 1, 2010): 52–69. http://dx.doi.org/10.5670/oceanog.2010.05.

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8

Liu, W. Timothy, Xiaosu Xie, and Pearn P. Niiler. "Ocean–Atmosphere Interaction over Agulhas Extension Meanders." Journal of Climate 20, no. 23 (December 1, 2007): 5784–97. http://dx.doi.org/10.1175/2007jcli1732.1.

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Abstract Many years of high-resolution measurements by a number of space-based sensors and from Lagrangian drifters became available recently and are used to examine the persistent atmospheric imprints of the semipermanent meanders of the Agulhas Extension Current (AEC), where strong surface current and temperature gradients are found. The sea surface temperature (SST) measured by the Advanced Microwave Scanning Radiometer-Earth Observing System (AMSR-E) and the chlorophyll concentration measured by the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) support the identification of the meanders and related ocean circulation by the drifters. The collocation of high and low magnitudes of equivalent neutral wind (ENW) measured by Quick Scatterometer (QuikSCAT), which is uniquely related to surface stress by definition, illustrates not only the stability dependence of turbulent mixing but also the unique stress measuring capability of the scatterometer. The observed rotation of ENW in opposition to the rotation of the surface current clearly demonstrates that the scatterometer measures stress rather than winds. The clear differences between the distributions of wind and stress and the possible inadequacy of turbulent parameterization affirm the need of surface stress vector measurements, which were not available before the scatterometers. The opposite sign of the stress vorticity to current vorticity implies that the atmosphere spins down the current rotation through momentum transport. Coincident high SST and ENW over the southern extension of the meander enhance evaporation and latent heat flux, which cools the ocean. The atmosphere is found to provide negative feedback to ocean current and temperature gradients. Distribution of ENW convergence implies ascending motion on the downwind side of local SST maxima and descending air on the upwind side and acceleration of surface wind stress over warm water (deceleration over cool water); the convection may escalate the contrast of ENW over warm and cool water set up by the dependence of turbulent mixing on stability; this relation exerts a positive feedback to the ENW–SST relation. The temperature sounding measured by the Atmospheric Infrared Sounder (AIRS) is consistent with the spatial coherence between the cloud-top temperature provided by the International Satellite Cloud Climatology Project (ISCCP) and SST. Thus ocean mesoscale SST anomalies associated with the persistent meanders may have a long-term effect well above the midlatitude atmospheric boundary layer, an observation not addressed in the past.
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9

Xie, Shang-Ping. "Satellite Observations of Cool Ocean–Atmosphere Interaction." Bulletin of the American Meteorological Society 85, no. 2 (February 1, 2004): 195–208. http://dx.doi.org/10.1175/bams-85-2-195.

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Over most of the World Ocean, sea surface temperature (SST) is below 26°C and atmospheric deep convection rarely takes place. Cool ocean–atmosphere interaction is poorly understood and this lack of understanding is a stumbling block in the current effort to study non-ENSO climate variability. Using new satellite observations, the response of surface wind and low clouds to changes in SST is investigated over cool oceans, where the planetary boundary layer (PBL) is often capped by a temperature inversion. While one-way atmospheric forcing is a major mechanism for basinscale SST variability in the extratropics, clear wind response is detected in regions of strong ocean currents. In particular, SST modulation of vertical momentum mixing emerges as the dominant mechanism for SST-induced wind variability near oceanic fronts around the world, which is characterized by a positive SST–wind speed correlation. Several types of boundary layer cloud response are found, whose correlation with SST varies from positive to negative, depending on the role of surface moisture convergence. Noting that the surface moisture convergence is strongly scale dependent, it is proposed that horizontal scale is important for setting the sign of this SST–cloud correlation. Finally, the processes by which a shallow PBL response might lead to a deep, tropospheric-scale response and the implications for the study of extratropical basin-scale air–sea interaction are discussed.
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10

Fleagle, R. G., N. A. Bond, and W. A. Nuss. "Atmosphere-ocean interaction in mid-latitude storms." Meteorology and Atmospheric Physics 38, no. 1-2 (1988): 50–63. http://dx.doi.org/10.1007/bf01029947.

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Дисертації з теми "Ocean-atmosphere interaction"

1

Seo, Hyodae. "Mesoscale coupled ocean-atmosphere interaction." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2007. http://wwwlib.umi.com/cr/ucsd/fullcit?p3263355.

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Thesis (Ph. D.)--University of California, San Diego, 2007.
Title from first page of PDF file (viewed July 10, 2007). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references (p. 138-152).
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2

Zhang, Yuan. "An observational study of atmosphere-ocean interactions in the northern oceans on interannual and interdecadal time-scale /." Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/10038.

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3

Helber, Robert William. "Upper ocean upwelling, temperature, and zonal momentum analyses in the western equatorail [sic] Pacific." [Tampa, Fla. : s.n.], 2003. http://purl.fcla.edu/fcla/etd/SFE0000073.

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Weinstein, Sarah Elizabeth. "Sources, transport, and fates of particulate trace metals in the Gulf of Maine-Scotian Shelf and Labrador Sea /." View online ; access limited to URI, 2003. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3115641.

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5

Kern, Bastian [Verfasser]. "Chemical interaction between ocean and atmosphere / Bastian Kern." Mainz : Universitätsbibliothek Mainz, 2014. http://d-nb.info/1060212412/34.

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6

Kochanski, Adam. "On the practical applications of atmosphere-ocean and atmosphere-wave coupling in mesoscale numerical modeling." abstract and full text PDF (UNR users only), 2008. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3316369.

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Eichelberger, Scott James. "The effects of meridional heating gradients on the atmospheric general circulation and its variability /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/10029.

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8

施錦杯 and Kam-pui Sze. "Effects of the interaction of atmosphere and ocean on humanactivities." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B31254378.

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9

Mosedale, Timothy James. "North Atlantic Ocean-atmosphere interaction using simple and complex models." Thesis, University of Reading, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.430918.

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10

Guo, Larsén Xiaoli. "Air-sea exchange of momentum and sensible heat over the Baltic Sea /." Uppsala : Acta Universitatis Upsaliensis : Univ.-bibl. [distributör], 2003. http://publications.uu.se/theses/91-554-5565-4/.

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Книги з теми "Ocean-atmosphere interaction"

1

Kraus, E. B. Atmosphere-ocean interaction. 2nd ed. New York: Oxford University Press, 1994.

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2

1931-, Toba Y., ed. Ocean-atmosphere interactions. Tokyo: Terra Scientific Pub. Co., 2003.

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3

Allan, Perrie William, ed. Atmosphere-ocean interactions. Southampton: WIT Press, 2002.

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4

Chunzai, Wang, Xie Shang-Ping, and Carton James A, eds. Earth's climate: The ocean-atmosphere interaction. Washington, DC: American Geophysical Union, 2004.

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5

Kagan, B. A. Ocean-atmosphere interaction and climate modelling. Cambridge [England]: Cambridge University Press, 1995.

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6

E, Schlesinger M., North Atlantic Treaty Organization, and Commission of the European Communities., eds. Climate-ocean interaction. Dordrecht, The Netherlands: Kluwer Academic Publishers, 1990.

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7

Corinne, Le Quéré, and Saltzman Eric S. 1955-, eds. Surface ocean-lower atmosphere processes. Washington, DC: American Geophysical Union, 2010.

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Le, Quéré Corinne, and Saltzman Eric S. 1955-, eds. Surface ocean-lower atmosphere processes. Washington, DC: American Geophysical Union, 2010.

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9

National Seminar on Antarctic Geoscience, Ocean-atmosphere Interaction and Paleoclimatology (2003 Velha Goa, India). Antarctic geoscience, ocean-atmosphere interaction and paleoclimatology. Edited by Rajan S, Pandey Prem Chand, and National Centre for Antarctic & Ocean Research (India). Goa: National Centre for Antarctic & Ocean Research, 2012.

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10

Liss, Peter S. Ocean-Atmosphere Interactions of Gases and Particles. Cham: Springer Nature, 2014.

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Частини книг з теми "Ocean-atmosphere interaction"

1

Battisti, David S. "Interannual Variability in Coupled Tropical Atmosphere-Ocean Models." In Climate-Ocean Interaction, 127–59. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-2093-4_7.

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2

Pedlosky, Joseph. "Wave-Mean Flow Interaction." In Waves in the Ocean and Atmosphere, 231–37. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_21.

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3

Lin, Charles A., Richard J. Greatbatch, and Sheng Zhang. "Large Scale Atmosphere-Ocean Interaction and Climate." In Climate Sensitivity to Radiative Perturbations, 291–303. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-61053-0_22.

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4

Lau, William K. M., Duane E. Waliser, and Harry Hendon. "Air–sea interaction." In Intraseasonal Variability in the Atmosphere-Ocean Climate System, 247–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-13914-7_7.

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5

Wang, Chunzai, Shang-Ping Xie, and James A. Carton. "Preface." In Earth's Climate: The Ocean-Atmosphere Interaction, vii. Washington, D. C.: American Geophysical Union, 2004. http://dx.doi.org/10.1029/147gm00.

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6

Lemke, Peter. "Stochastic Description of Atmosphere — Sea Ice — Ocean Interaction." In The Geophysics of Sea Ice, 785–823. Boston, MA: Springer US, 1986. http://dx.doi.org/10.1007/978-1-4899-5352-0_14.

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Lau, William K. M., Duane E. Waliser, and Jean Philippe Duvel. "Oceans and air–sea interaction." In Intraseasonal Variability in the Atmosphere-Ocean Climate System, 513–36. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-13914-7_15.

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8

Lunine, Jonathan I., and David J. Stevenson. "Evolution of Titan’s Coupled Ocean-Atmosphere System and Interaction of Ocean with Bedrock." In Ices in the Solar System, 741–57. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5418-2_50.

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9

Wang, Chunzai, Shang-Ping Xie, and James A. Carton. "A Global Survey of Ocean-Atmosphere Interaction and Climate Variability." In Earth's Climate, 1–19. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/147gm01.

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10

Grankov, Alexander, and Alexander Milshin. "Effectiveness of the Satellite MCW Radiometric Means of Studying the Air–Sea Interaction." In Natural Microwave Radiation of the Ocean-Atmosphere System, 123–54. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3206-5_5.

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Тези доповідей конференцій з теми "Ocean-atmosphere interaction"

1

Lee, Han Soo, and Takao Yamshita. "NUMERICAL EXPERIMENTS ON TYPHOON AND OCEAN INTERACTION BY ATMOSPHERE-OCEAN COUPLED MODEL." In Proceedings of the 31st International Conference. World Scientific Publishing Company, 2009. http://dx.doi.org/10.1142/9789814277426_0098.

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2

Thien, Le Van. "OCEAN-ATMOSPHERE INTERACTION OVER UPWELING REGION OFF CENTRAL VIETNAM: OBSERVATION STUDY." In NGHIÊN CỨU CƠ BẢN TRONG LĨNH VỰC KHOA HỌC TRÁI ĐẤT VÀ MÔI TRƯỜNG. Publishing House for Science and Technology, 2019. http://dx.doi.org/10.15625/vap.2019.000138.

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3

Witthuhn, Jonas, Anja Hünerbein, Florian Filipitsch, Stefan Wacker, Stefanie Meilinger, and Hartwig Deneke. "Aerosol properties and aerosol–radiation interaction in clear-skies over Germany for the period from 2003 to 2020." In RADIATION PROCESSES IN THE ATMOSPHERE AND OCEAN. AIP Publishing, 2024. http://dx.doi.org/10.1063/5.0184865.

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4

Shuvalova, Julia, Natalia Chubarova, and Marina Shatunova. "Solar irradiance and cloud-radiation interaction according to the ICON-Ru and COSMO-Ru simulations, ground-based and satellite observations." In RADIATION PROCESSES IN THE ATMOSPHERE AND OCEAN. AIP Publishing, 2024. http://dx.doi.org/10.1063/5.0182766.

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5

Jensen, T. G., W. E. Rogers, U. Gravois, T. Campbell, and R. Allard. "Wave-current interaction in the Florida Current in a coupled atmosphere-ocean-wave model." In OCEANS 2011. IEEE, 2011. http://dx.doi.org/10.23919/oceans.2011.6107015.

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Rasheed, Adil, Jakob Kristoffer Süld, and Mandar Tabib. "Effect of Uni- and Bi-Directional Coupling of Ocean-Met Interaction on Significant Wave Height and Local Wind." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61681.

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Accurate prediction of near surface wind and wave height are important for many offshore activities like fishing, boating, surfing, installation and maintenance of marine structures. The current work investigates the use of different methodologies to make accurate predictions of significant wave height and local wind. The methodology consists of coupling an atmospheric code HARMONIE and a wave model WAM. Two different kinds of coupling methodologies: unidirectional and bidirectional coupling are tested. While in Unidirectional coupling only the effects of atmosphere on ocean surface are taken into account, in bidirectional coupling the effects of ocean surface on the atmosphere are also accounted for. The predicted values of wave height and local wind at 10m above the ocean surface using both the methodologies are compared against observation data. The results show that during windy conditions, a bidirectional coupling methodology has better prediction capability.
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"Understanding the Interaction of Land, Ocean and Atmosphere: Disaster Mitigation and Regional Resillience [Front cover]." In 2020 IEEE Asia-Pacific Conference on Geoscience, Electronics and Remote Sensing Technology (AGERS). IEEE, 2020. http://dx.doi.org/10.1109/agers51788.2020.9452787.

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Grankov, Alexander G., Alexander A. Mil'shin, and Vladimir F. Krapivin. "Intercorrelation between natural microwave radiation of the ocean-atmosphere system and its boundary heat and dynamic interaction." In SPIE Europe Remote Sensing, edited by Charles R. Bostater, Jr., Stelios P. Mertikas, Xavier Neyt, and Miguel Velez-Reyes. SPIE, 2009. http://dx.doi.org/10.1117/12.834939.

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Sekiguchi, Miho, Takashi Y. Nakajima, Takashi M. Nagao, and Teruyuki Nakajima. "Regional properties of aerosol-cloud interaction estimated from long-term satellite analysis." In RADIATION PROCESSES IN THE ATMOSPHERE AND OCEAN (IRS2016): Proceedings of the International Radiation Symposium (IRC/IAMAS). Author(s), 2017. http://dx.doi.org/10.1063/1.4975507.

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Pan, Xiaoling, Wei Gao, Fengxue Gu, Weiqing Li, Shunli Chang, Yuandong Zhang, Qian Ye, and Subai Anabiek. "The evaluation on interaction between structures and succession of vegetation/ecosystems and arid land environment in western China: a case study on Fukang, Xinjiang." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Xiaoling Pan, Wei Gao, Michael H. Glantz, and Yoshiaki Honda. SPIE, 2003. http://dx.doi.org/10.1117/12.466609.

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Звіти організацій з теми "Ocean-atmosphere interaction"

1

Zappa, Christopher J. Ocean Surface Temperature Response to Atmosphere-Ocean Interaction of the MJO. Fort Belvoir, VA: Defense Technical Information Center, September 2011. http://dx.doi.org/10.21236/ada557074.

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Zappa, Christopher J., and Arnold L. Gordon. Atmosphere-Ocean Interaction of the MJO from Unmanned Airborne Vehicles. Fort Belvoir, VA: Defense Technical Information Center, September 2011. http://dx.doi.org/10.21236/ada553770.

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Flatau, Maria, Toshiaki Shinoda, Sue Chen, and Tommy Jensen. The Influence of Atmosphere-Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada574456.

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Flatau, Maria, Toshiaki Shinoda, Sue Chen, and Tommy Jensen. The Influence of Atmosphere-Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada575530.

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Chen, Sue, James D. Doyle, Paul May, and Jerome M. Schmidt. The Influence of Atmosphere-Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2013. http://dx.doi.org/10.21236/ada598118.

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Flatau, Maria, Toshiaki Shinoda, Sue Chen, and Tommy Jensen. The Influence of Atmosphere-Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2013. http://dx.doi.org/10.21236/ada598808.

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Flatau, Maria, Toshiaki Shinoda, Sue Chen, and Tommy Jensen. The Influence of Atmosphere - Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2011. http://dx.doi.org/10.21236/ada557129.

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Flatau, Maria, Toshiaki Shinoda, Sue Chen, and Tommy Jensen. The Influence of Atmosphere-Ocean Interaction on MJO Development and Propagation. Fort Belvoir, VA: Defense Technical Information Center, September 2014. http://dx.doi.org/10.21236/ada616719.

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9

Stanley, Rachel H. R., Thomas Thomas, Yuan Gao, Cassandra Gaston, David Ho, David Kieber, Kate Mackey, et al. US SOLAS Science Report. Woods Hole Oceanographic Institution, December 2021. http://dx.doi.org/10.1575/1912/27821.

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Анотація:
The Surface Ocean – Lower Atmosphere Study (SOLAS) (http://www.solas-int.org/) is an international research initiative focused on understanding the key biogeochemical-physical interactions and feedbacks between the ocean and atmosphere that are critical elements of climate and global biogeochemical cycles. Following the release of the SOLAS Decadal Science Plan (2015-2025) (Brévière et al., 2016), the Ocean-Atmosphere Interaction Committee (OAIC) was formed as a subcommittee of the Ocean Carbon and Biogeochemistry (OCB) Scientific Steering Committee to coordinate US SOLAS efforts and activities, facilitate interactions among atmospheric and ocean scientists, and strengthen US contributions to international SOLAS. In October 2019, with support from OCB, the OAIC convened an open community workshop, Ocean-Atmosphere Interactions: Scoping directions for new research with the goal of fostering new collaborations and identifying knowledge gaps and high-priority science questions to formulate a US SOLAS Science Plan. Based on presentations and discussions at the workshop, the OAIC and workshop participants have developed this US SOLAS Science Plan. The first part of the workshop and this Science Plan were purposefully designed around the five themes of the SOLAS Decadal Science Plan (2015-2025) (Brévière et al., 2016) to provide a common set of research priorities and ensure a more cohesive US contribution to international SOLAS.
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Rogers, David P. Coupled Ocean-Atmosphere Interaction and the Development of the Marine Atmospheric Boundary Layer. Fort Belvoir, VA: Defense Technical Information Center, October 1997. http://dx.doi.org/10.21236/ada330047.

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