Relevant bibliographies by topics / Land surface atmosphere feedback

Contents

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

Academic literature on the topic 'Land surface atmosphere feedback'

Author: Grafiati
Published: 4 June 2021
Last updated: 11 February 2022

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Journal articles on the topic "Land surface atmosphere feedback"

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Tuinenburg, O. A., R. W. A. Hutjes, C. M. J. Jacobs, and P. Kabat. "Diagnosis of Local Land–Atmosphere Feedbacks in India." Journal of Climate 24, no. 1 (2011): 251–66. http://dx.doi.org/10.1175/2010jcli3779.1.

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Abstract Following the convective triggering potential (CTP)–humidity index (HIlow) framework by Findell and Eltahir, the sensitivity of atmospheric convection to soil moisture conditions is studied for India. Using the same slab model as Findell and Eltahir, atmospheric conditions in which the land surface state affects convective precipitation are determined. For India, CTP–HIlow thresholds for land surface–atmosphere feedbacks are shown to be slightly different than for the United States. Using atmospheric sounding data from 1975 to 2009, the seasonal and spatial variations in feedback stre
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Zabel, F., W. Mauser, T. Marke, A. Pfeiffer, G. Zängl, and C. Wastl. "Inter-comparison of two land-surface schemes applied on different scales and their feedbacks while coupled with a regional climate model." Hydrology and Earth System Sciences Discussions 8, no. 4 (2011): 7091–136. http://dx.doi.org/10.5194/hessd-8-7091-2011.

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Abstract. Feedback effects between the land surface and the atmosphere are an important issue in modelling the climate system. Therefore, in order to take land surface heterogeneity adequately into account, a representation of the land surface in sufficient spatial resolution is necessary. In order to analyze the impact of different land surface models on the atmosphere, we analyzed the differences of two physically based land surface models, which evolved from different disciplinary backgrounds, both fully coupled with the regional climate model MM5, providing the atmospheric drivers. While t
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Koster, Randal D., Yehui Chang, and Siegfried D. Schubert. "A Mechanism for Land–Atmosphere Feedback Involving Planetary Wave Structures." Journal of Climate 27, no. 24 (2014): 9290–301. http://dx.doi.org/10.1175/jcli-d-14-00315.1.

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Abstract While the ability of land surface conditions to influence the atmosphere has been demonstrated in various modeling and observational studies, the precise mechanisms by which land–atmosphere feedback occurs are still largely unknown: particularly the mechanisms that allow land moisture state in one region to affect atmospheric conditions in another. Such remote impacts are examined here in the context of atmospheric general circulation model (AGCM) simulations, leading to the identification of one potential mechanism: the phase locking and amplification of a planetary wave through the
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Dirmeyer, Paul A., Randal D. Koster, and Zhichang Guo. "Do Global Models Properly Represent the Feedback between Land and Atmosphere?" Journal of Hydrometeorology 7, no. 6 (2006): 1177–98. http://dx.doi.org/10.1175/jhm532.1.

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Abstract The Global Energy and Water Cycle Experiment/Climate Variability and Predictability (GEWEX/CLIVAR) Global Land–Atmosphere Coupling Experiment (GLACE) has provided an estimate of the global distribution of land–atmosphere coupling strength during boreal summer based on the results from a dozen weather and climate models. However, there is a great deal of variation among models, attributable to a range of sensitivities in the simulation of both the terrestrial and atmospheric branches of the hydrologic cycle. It remains an open question whether any of the models, or the multimodel estim
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Santanello, Joseph A., Mark A. Friedl, and Michael B. Ek. "Convective Planetary Boundary Layer Interactions with the Land Surface at Diurnal Time Scales: Diagnostics and Feedbacks." Journal of Hydrometeorology 8, no. 5 (2007): 1082–97. http://dx.doi.org/10.1175/jhm614.1.

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Abstract The convective planetary boundary layer (PBL) integrates surface fluxes and conditions over regional and diurnal scales. As a result, the structure and evolution of the PBL contains information directly related to land surface states. To examine the nature and magnitude of land–atmosphere coupling and the interactions and feedbacks controlling PBL development, the authors used a large sample of radiosonde observations collected at the southern Atmospheric Research Measurement Program–Great Plains Cloud and Radiation Testbed (ARM-CART) site in association with simulations of mixed-laye
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Stap, Lennert B., Bart J. J. M. van den Hurk, Chiel C. van Heerwaarden, and Roel A. J. Neggers. "Modeled Contrast in the Response of the Surface Energy Balance to Heat Waves for Forest and Grassland." Journal of Hydrometeorology 15, no. 3 (2014): 973–89. http://dx.doi.org/10.1175/jhm-d-13-029.1.

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Abstract Observations have shown that differences in surface energy fluxes over grasslands and forests are amplified during heat waves. The role of land–atmosphere feedbacks in this process is still uncertain. In this study, a single-column model (SCM) is used to investigate the difference between forest and grassland in their energy response to heat waves. Three simulations for the period 2005–11 were carried out: a control run using vegetation characteristics for Cabauw (the Netherlands), a run where the vegetation is changed to 100% forest, and a run with 100% short grass as vegetation. A s
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Chen, Haishan, Bo Yu, Botao Zhou, Wanxin Zhang, and Jie Zhang. "Role of Local Atmospheric Forcing and Land–Atmosphere Interaction in Recent Land Surface Warming in the Midlatitudes over East Asia." Journal of Climate 33, no. 6 (2020): 2295–309. http://dx.doi.org/10.1175/jcli-d-18-0856.1.

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AbstractSignificant summer land surface warming has been observed in the middle latitudes over East Asia, especially after the mid-1990s, which has evidently affected the East Asian weather and climate. Using multisource observations and reanalysis data during 1979–2013, this study explores the possible reasons for recent land surface warming over this region by considering atmospheric forcing and regional land–atmosphere interaction related to extratropical cyclones (ECs). Results show that there is a close relationship between land surface warming and weakened ECs over East Asia. Recent land
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Laguë, Marysa M., Gordon B. Bonan, and Abigail L. S. Swann. "Separating the Impact of Individual Land Surface Properties on the Terrestrial Surface Energy Budget in both the Coupled and Uncoupled Land–Atmosphere System." Journal of Climate 32, no. 18 (2019): 5725–44. http://dx.doi.org/10.1175/jcli-d-18-0812.1.

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Abstract Changes in the land surface can drive large responses in the atmosphere on local, regional, and global scales. Surface properties control the partitioning of energy within the surface energy budget to fluxes of shortwave and longwave radiation, sensible and latent heat, and ground heat storage. Changes in surface energy fluxes can impact the atmosphere across scales through changes in temperature, cloud cover, and large-scale atmospheric circulation. We test the sensitivity of the atmosphere to global changes in three land surface properties: albedo, evaporative resistance, and surfac
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Levine, Paul A., James T. Randerson, Sean C. Swenson, and David M. Lawrence. "Evaluating the strength of the land–atmosphere moisture feedback in Earth system models using satellite observations." Hydrology and Earth System Sciences 20, no. 12 (2016): 4837–56. http://dx.doi.org/10.5194/hess-20-4837-2016.

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Abstract. The relationship between terrestrial water storage (TWS) and atmospheric processes has important implications for predictability of climatic extremes and projection of future climate change. In places where moisture availability limits evapotranspiration (ET), variability in TWS has the potential to influence surface energy fluxes and atmospheric conditions. Where atmospheric conditions, in turn, influence moisture availability, a full feedback loop exists. Here we developed a novel approach for measuring the strength of both components of this feedback loop, i.e., the forcing of the
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Williams, John L., and Reed M. Maxwell. "Propagating Subsurface Uncertainty to the Atmosphere Using Fully Coupled Stochastic Simulations." Journal of Hydrometeorology 12, no. 4 (2011): 690–701. http://dx.doi.org/10.1175/2011jhm1363.1.

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Abstract Feedbacks between the land surface and the atmosphere, manifested as mass and energy fluxes, are strongly correlated with soil moisture, making soil moisture an important factor in land–atmosphere interactions. It is shown that a reduction of the uncertainty in subsurface properties such as hydraulic conductivity (K) propagates into the atmosphere, resulting in a reduction in uncertainty in land–atmosphere feedbacks that yields more accurate atmospheric predictions. Using the fully coupled groundwater-to-atmosphere model ParFlow-WRF, which couples the hydrologic model ParFlow with the
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Dissertations / Theses on the topic "Land surface atmosphere feedback"

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Häntzschel, Janet. "Untersuchungen zur Landoberflächenrückkopplung der Atmosphäre und ihrer Auswirkung auf den Wasserhaushalt." Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2005. http://nbn-resolving.de/urn:nbn:de:swb:14-1134722228059-54242.

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Die vorliegende Arbeit hat zum Ziel, den Einfluss der Rückkopplung zwischen Landoberfläche und Atmosphäre auf den regionalen Wasserhaushalt abzuschätzen. Dazu erfolgen Modellsimulationen mit dem gekoppelten Vegetations-Grenzschichtmodell HIRVAC (HIgh Resolution Vegetation Atmosphere Coupler) für das Einzugsgebiet Sperrgraben (Bayerische Alpen). Im Ergebnis wird der Zusammenhang zwischen dem Entkopplungsfaktor Omega und der Verdunstung als Wasserhaushaltsgröße für einen festgelegten Zeitraum untersucht. Die Kombination eines vertikal hochaufgelösten Grenzschichtmodells (HUB) mit einem mechanist
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White, Cary Blake, and Cary Blake White. "Soil Moisture Variability in Land Surface-Atmosphere Interactions." Thesis, The University of Arizona, 1996. http://hdl.handle.net/10150/626791.

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Meteorological measurements in the Walnut Gulch catchment in Arizona were used to synthesize a distributed, hourly-average time series of data across a 26.9 by 12.5 km area with a grid resolution of 480 m for a continuous 18-month period which included two seasons of monsoonal rainfall. Coupled surface-atmosphere model runs established the acceptability (for modeling purposes) of assuming uniformity in all meteorological variables other than rainfall. Rainfall was interpolated onto the grid from an array of 82 recording rain gauges. These meteorological data were used as forcing va
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Liu, Yuqiong. "Parameter Estimations For Locally Coupled Land Surface-Atmosphere Models." Diss., The University of Arizona, 2003. http://hdl.handle.net/10150/191262.

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As land-surface modeling moves from the off-line mode to the coupled mode, it is also highly desirable to extend the off-line calibration of land-surface models to coupled applications. Using the NCAR SCCM as an example, this study proposed and implemented some effective schemes for the application of automatic parameter estimation procedures in a locally coupled environment, where other relevant issues such as parameterization tests, sensitivity analyses, and off-line calibrations were also involved. A parameterization deficiency having serious negative impacts on the performance of the NCAR
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Ghent, Darren John. "Land surface modelling and Earth observation of land/atmosphere interactions in African savannahs." Thesis, University of Leicester, 2011. http://hdl.handle.net/2381/10274.

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Land/atmosphere feedback processes play a significant role in determining climate forcing on monthly to decadal timescales. Considerable uncertainty however exists in land surface model representation of these processes. This investigation represents an innovative approach to understanding key land surface processes in African savannahs in the framework of the UK‘s most important land surface model – the Joint UK Land Environment Simulator (JULES). Findings from an investigation into the carbon balance of Africa for a 25-year period from 1982 to 2006 inclusive show that JULES estimated Africa
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Goncalves, de Goncalves Luis Gustavo. "LAND SURFACE-ATMOSPHERE INTERACTIONS IN REGIONAL MODELING OVER SOUTH AMERICA." Diss., The University of Arizona, 2005. http://hdl.handle.net/10150/195893.

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Land surface processes play an important role when modeling weather and climate, and understanding and representing such processes in South America is a particular challenge because of the large variations in regional climate and surface features such as vegetation and soil. Numerical models have been used to explore the climate and weather of continental South America, but without appropriate initiation of land surface conditions model simulations can rapidly diverge from reality. This initiation problem is exacerbated by the fact that conventional surface observations over South America are
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Franks, Stewart William. "The representation of land surface - atmosphere fluxes for atmospheric modelling." Thesis, Lancaster University, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.387430.

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Zabel, Florian. "Land-atmosphere coupling between a land surface hydrological model and a regional climate model." Diss., lmu, 2012. http://nbn-resolving.de/urn:nbn:de:bvb:19-151446.

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Bain, Caroline Louise. "Interactions between the Land Surface and the Atmosphere over West Africa." Thesis, University of Leeds, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.491661.

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The north-south gradient in surface temperature and rainfall in West Africa leads to the summertime monsoon circulation. Here, the full extent of the relationship between the land surface and the atmosphere is discussed with particular reference to the impact that soil moisture has on the atmosphere at different spatial scales. Observations from the AMMA field campaign in 2005 and 2006 are combined with satellite analysis and model simulations to discuss various interactions between the land surface and the atmosphere. Tethered balloon observations from Mali in August 2005 are used to assess t
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Manrique-Sunen, A. "The treatment of vegetation in land surface models : implications for predictions of land-atmosphere exchange." Thesis, University of Reading, 2016. http://centaur.reading.ac.uk/68719/.

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Plant processes affect fluxes of energy, moisture and CO2 between the land and the atmosphere. Land surface models need to correctly represent the vegetation functioning and its response to environmental conditions. Due to anthropogenic carbon emissions rising, and global warming, plant processes are being affected and in turn modulate the terrestrial carbon sink. However, models still disagree on the response of plants to changing conditions. This work analyses how vegetation is treated in two land surface models: the Joint UK Land Environment Simulator (JULES) and Carbon Hydrology Tiled ECMW
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McAtee, Brendon Kynnie. "Surface-atmosphere interactions in the thermal infrared (8 - 14um)." Curtin University of Technology, Department of Applied Physics, 2003. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=14481.

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Remote sensing of land surface temperature (LST) is a complex task. From a satellite-based perspective the radiative properties of the land surface and the atmosphere are inextricably linked. Knowledge of both is required if one is to accurately measure the temperature of the land surface from a space-borne platform. In practice, most satellite-based sensors designed to measure LST over the surface of the Earth are polar orbiting. They scan swaths of the order of 2000 km, utilizing zenith angles of observation of up to 60°. As such, satellite viewing geometry is important when comparing estima
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Books on the topic "Land surface atmosphere feedback"

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Wood, Eric F., ed. Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9.

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Labgaa, Rachid R. A model of the CO2 exchanges between biosphere and atmosphere in the tundra. Earth-Space Research Group, CRSEO -- Ellison Hall, University of California Santa Barbara, 1994.

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Mölder, Meelis. Parameterization of the interaction between the atmosphere and the land surface by means of roughness lengths: An experimental study over various surfaces. Sveriges lantbruksuniversitet, Institutionen för ekologi och miljövård, 1993.

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Claussen, Martin, Anne Dallmeyer, and Jürgen Bader. Theory and Modeling of the African Humid Period and the Green Sahara. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.532.

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There is ample evidence from palaeobotanic and palaeoclimatic reconstructions that during early and mid-Holocene between some 11,700 years (in some regions, a few thousand years earlier) and some 4200 years ago, subtropical North Africa was much more humid and greener than today. This African Humid Period (AHP) was triggered by changes in the orbital forcing, with the climatic precession as the dominant pacemaker. Climate system modeling in the 1990s revealed that orbital forcing alone cannot explain the large changes in the North African summer monsoon and subsequent ecosystem changes in the
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F, Wood Eric, ed. Land surface, atmosphere interactions for climate modeling: Observations, models, and analysis. Kluwer Academic Publishers, 1990.

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United States. National Aeronautics and Space Administration., ed. Differentiating the role of land surface variability and cloudiness variability on global energy transport within the atmosphere and oceans. National Aeronautics and Space Administration, 1993.

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Wood, E. F. Land Surface-Atmosphere Interactions for Climate Modeling: Observations, Models and Analysis (Reprinted from Surveys in Geophysics, Vol 12, Nos 1-3). Springer, 1990.

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1952-, Clifford Stephen Mark, Haberele Robert M, and Lunar and Planetary Institute, eds. MECA Workshop on Atmospheric H₂O Observations of Earth and Mars: Physical processes, measurements, and interpretations. The Institute ; [Springfield, Va., 1988.

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Palmer, Paul I. The Atmosphere: A Very Short Introduction. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780198722038.001.0001.

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The atmosphere is the thin, diffuse fluid that envelops the Earth’s surface. Despite its apparent fragility, the existence of this fluid is vital for human and other life on Earth. The Atmosphere: A Very Short Introduction describes the physical and chemical characteristics of different layers in the atmosphere, and shows how the atmosphere’s interactions with land, ocean, and ice affect these properties. It also looks at how movement in the atmosphere, driven by heat from the Sun, transports heat from lower latitudes to higher latitudes. Finally, it presents an overview of the types of measur
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Xue, Yongkang, Yaoming Ma, and Qian Li. Land–Climate Interaction Over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.592.

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The Tibetan Plateau (TP) is the largest and highest plateau on Earth. Due to its elevation, it receives much more downward shortwave radiation than other areas, which results in very strong diurnal and seasonal changes of the surface energy components and other meteorological variables, such as surface temperature and the convective atmospheric boundary layer. With such unique land process conditions on a distinct geomorphic unit, the TP has been identified as having the strongest land/atmosphere interactions in the mid-latitudes.Three major TP land/atmosphere interaction issues are presented
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Book chapters on the topic "Land surface atmosphere feedback"

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Holtslag, A. A. M., G. J. Steeneveld, and B. J. H. van de Wiel. "Role of land-surface temperature feedback on model performance for the stable boundary layer." In Atmospheric Boundary Layers. Springer New York, 2007. http://dx.doi.org/10.1007/978-0-387-74321-9_14.

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Zittis, G., P. Hadjinicolaou, and J. Lelieveld. "Land-Atmosphere Coupling: The Feedback of Soil Moisture into Surface Temperature in Eastern Mediterranean and Middle East." In Advances in Meteorology, Climatology and Atmospheric Physics. Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-29172-2_117.

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Xie, Zhenghui, Xiangjun Tian, Peihua Qin, et al. "Land Surface Improvements." In Flexible Global Ocean-Atmosphere-Land System Model. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-41801-3_45.

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O’Kane, J. Philip. "Implications for Remote Sensing of Natural Switching from Atmosphere-Controlled to Soil-Controlled Evaporation or Infiltration." In Land Surface Evaporation. Springer New York, 1991. http://dx.doi.org/10.1007/978-1-4612-3032-8_23.

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Royer, J. F. "Land Surface Processes and Hydrology." In Numerical Modeling of the Global Atmosphere in the Climate System. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-011-4046-1_13.

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Famiglietti, J. S., and E. F. Wood. "Evapotranspiration and Runoff from Large Land Areas: Land Surface Hydrology for Atmospheric General Circulation Models." In Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9_9.

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Shuttleworth, W. James. "Insight from Large-Scale Observational Studies of Land/Atmosphere Interactions." In Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9_1.

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Entekhabi, Dara, and Peter S. Eagleson. "Climate and the Equilibrium State of Land Surface Hydrology Parameterizations." In Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9_10.

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Kuhnel, V., J. C. I. Dooge, J. P. J. O’Kane, and R. J. Romanowicz. "Partial Analysis Applied to Scale Problems in Surface Moisture Fluxes." In Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9_11.

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Band, Lawrence E. "Distributed Parameterization of Complex Terrain." In Land Surface — Atmosphere Interactions for Climate Modeling. Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-009-2155-9_12.

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Conference papers on the topic "Land surface atmosphere feedback"

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Bedoya-Soto, Juan Mauricio, and Germán Poveda. "New insights on land surface-atmosphere feedbacks over tropical South America at interannual timescales." In First International Electronic Conference on the Hydrological Cycle. MDPI, 2017. http://dx.doi.org/10.3390/chycle-2017-04875.

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Nowak, Dariusz, Valter Bellucci, Jan Cerny, and Geoffrey Engelbrecht. "Numerical Modeling of Thermoacoustic Oscillations in a Gas Turbine Combustion Chamber." In ASME Turbo Expo 2006: Power for Land, Sea, and Air. ASMEDC, 2006. http://dx.doi.org/10.1115/gt2006-90945.

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The prediction of high-frequency acoustic oscillations in gas turbine combustors is an important issue, related to engine performance, NOx emissions, component lifetime and engine operational flexibility. Different methods with increasing complexity and predictive ability have been discussed in a number of papers. Application of these methods requires large computational capacity and long computational times. Therefore, a limited number of variants of small combustor models or small sectors can be analyzed in a reasonable time. This paper presents an approximate approach, applicable under cert
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Galve, J. M., C. Coll, V. Caselles, et al. "A Cloudless land atmosphere radiosounding database for generating land surface temperature retrieval algorithms." In 2007 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2007. http://dx.doi.org/10.1109/igarss.2007.4423196.

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DeSlover, Daniel H., Robert O. Knuteson, Brian Osborne, Daniel K. Zhou, and William L. Smith. "Validation of aircraft-measured land surface emissivity." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Hung-Lung Huang, Daren Lu, and Yasuhiro Sasano. SPIE, 2003. http://dx.doi.org/10.1117/12.466041.

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Zhan, Chuan, Bo-Hui Tang, Hua Wu, Ronglin Tang, and Zhao-Liang Li. "Analyzing the influence of anomalous atmosphere on land surface temperature retrieval." In IGARSS 2016 - 2016 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2016. http://dx.doi.org/10.1109/igarss.2016.7730119.

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Avissar, Roni. "Bridging the gap between microscale land-surface processes and land-atmosphere interactions at the scale of GCM’s." In The world at risk: Natural hazards and climate change. AIP, 1992. http://dx.doi.org/10.1063/1.43902.

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Knuteson, Robert O., Daniel H. Deslover, Allen M. Larar, et al. "Infrared land surface remote sensing using high spectral resolution observations." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Allen M. Larar, Qingxi Tong, and Makoto Suzuki. SPIE, 2003. http://dx.doi.org/10.1117/12.467425.

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Xu, Jiafei, Zhengchao Chen, Hao Zhang, Bing Zhang, and Tao Liu. "Preliminary validation of GF-1/GF-2 surface reflectance products over land using VNIR atmospheric correction method." In Remote Sensing of Clouds and the Atmosphere XXIV, edited by Adolfo Comerón, Evgueni I. Kassianov, Klaus Schäfer, Richard H. Picard, Konradin Weber, and Upendra N. Singh. SPIE, 2019. http://dx.doi.org/10.1117/12.2535792.

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Babanin, Alexander V. "Wave-Induced Turbulence, Linking Metocean and Large Scales." In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-18373.

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Abstract Until recently, large-scale models did not explicitly take account of ocean surface waves which are a process of much smaller scales. However, it is rapidly becoming clear that many large-scale geophysical processes are essentially coupled with the surface waves, and those include ocean circulation, weather, Tropical Cyclones and polar sea ice in both Hemispheres, climate and other phenomena in the atmosphere, at air/sea, sea/ice and sea/land interface, and many issues of the upper-ocean mixing below the surface. Besides, the wind-wave climate itself experiences large-scale trends and
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Chen, Haishan, and Zhaobo Sun. "Point simulation of seasonal snow cover with comprehensive land surface model." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Zhaobo Sun, Fei-Fei Jin, and Toshiki Iwasaki. SPIE, 2003. http://dx.doi.org/10.1117/12.466688.

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Reports on the topic "Land surface atmosphere feedback"

1

Gutowski, W. J. Jr. Modeling land-surface/atmosphere dynamics for CHAMMP. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/6711123.

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Jakubiak, Bogumil, Teddy Holt, Richard Hodur, Maciej Szpindler, and Leszek Herman-Izycki. Implementation of Modeling the Land-Surface/Atmosphere Interactions to Mesoscale Model COAMPS. Defense Technical Information Center, 2010. http://dx.doi.org/10.21236/ada541836.

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Jakubiak, Bogumil, Teddy Holt, Richard Hodur, Maciej Szpindler, and Leszek Herman-Izycki. Implementation of Modeling the Land-Surface/Atmosphere Interactions to Mesoscale Model COAMPS. Defense Technical Information Center, 2011. http://dx.doi.org/10.21236/ada557104.

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Jakubiak, Bogumil, Richard Hodur, and Leszek Herman-Izycki. Implementation of Modeling the Land-Surface/Atmosphere Interactions to Mesoscale Model COAMPS. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada574482.

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5

Gutowski, W. J. Jr. Modeling land-surface/atmosphere dynamics for CHAMMP. Progress report, August 1, 1992--31 July 1993. Office of Scientific and Technical Information (OSTI), 1993. http://dx.doi.org/10.2172/10128173.

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6

Sumant Nigam. Atmosphere-Land-Surface Interaction over the Southern Great Plains: Diagnosis of Mechanisms from SGP ARM Data. Office of Scientific and Technical Information (OSTI), 2013. http://dx.doi.org/10.2172/1061466.

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