Bibliografías temáticas / Forest-Atmosphere exchanges

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Literatura académica sobre el tema "Forest-Atmosphere exchanges"

Autor: Grafiati
Publicado: 21 de diciembre de 2024
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "Forest-Atmosphere exchanges"

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Serra-Neto, Edivaldo M., Hardiney S. Martins, Cléo Q. Dias-Júnior, et al. "Simulation of the Scalar Transport above and within the Amazon Forest Canopy." Atmosphere 12, no. 12 (2021): 1631. http://dx.doi.org/10.3390/atmos12121631.

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The parallelized large-eddy simulation model (PALM) was used to understand better the turbulent exchanges of a passive scalar above and within a forested region located in the central Amazon. Weak (2 ms−1) and strong (6 ms−1) wind conditions were simulated. A passive scalar source was introduced to the forest floor for both simulations. The simulations reproduced the main characteristics of the turbulent flow and of the passive scalar transport between the forest and the atmosphere. Noteworthily, strong and weak wind conditions presented different turbulence structures that drove different pat
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Wiedinmyer, Christine, Michael Barlage, Mukul Tewari, and Fei Chen. "Meteorological Impacts of Forest Mortality due to Insect Infestation in Colorado." Earth Interactions 16, no. 2 (2012): 1–11. http://dx.doi.org/10.1175/2011ei419.1.

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Abstract Physical characteristics of forests and other ecosystems control land–atmosphere exchanges of water and energy and partly dictate local and regional meteorology. Insect infestation and resulting forest dieback can alter these characteristics and, further, modify land–atmosphere exchanges. In the past decade, insect infestation has led to large-scale forest mortality in western North America. This study uses a high-resolution mesoscale meteorological model coupled with a detailed land surface model to investigate the sensitivity of near-surface variables to insect-related forest mortal
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Pinheiro, Di Angelo Matos, Cléo Quaresma Dias-Júnior, Leonardo Deane de Abreu Sá, and Antonio Ocimar Manzi. "Usando a altura do ponto de inflexão no perfil do vento para a obtenção de perfis adimensionais acima da floresta amazônica." Ciência e Natura 42 (August 28, 2020): e24. http://dx.doi.org/10.5902/2179460x53225.

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The most turbulent vortices that populate the forest-atmosphere interface have canopy height length scales. These vortices are mainly responsible for turbulent exchanges between inside and above canopy region. Thus, we used the vertical wind profiles obtained by 10 anemometers installed inside and above the forest canopy of the Rebio-Jarú experimental site, in the Amazon Rainforest. A third degree polynomial function was developed to better fit the wind profile and therefore estimate the inflection point height of the vertical wind profile (zi) a length scale associated with wind shear (Ls), a
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4

Smallman, T. L., J. B. Moncrieff, and M. Williams. "WRFv3.2-SPAv2: development and validation of a coupled ecosystem–atmosphere model, scaling from surface fluxes of CO<sub>2</sub> and energy to atmospheric profiles." Geoscientific Model Development 6, no. 4 (2013): 1079–93. http://dx.doi.org/10.5194/gmd-6-1079-2013.

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Abstract. The Weather Research and Forecasting meteorological (WRF) model has been coupled to the Soil–Plant–Atmosphere (SPA) terrestrial ecosystem model, to produce WRF-SPA. SPA generates realistic land–atmosphere exchanges through fully coupled hydrological, carbon and energy cycles. The addition of a~land surface model (SPA) capable of modelling biospheric CO2 exchange allows WRF-SPA to be used for investigating the feedbacks between biosphere carbon balance, meteorology, and land use and land cover change. We have extensively validated WRF-SPA using multi-annual observations of air tempera
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Smallman, T. L., J. B. Moncrieff, and M. Williams. "WRFv3.2-SPAv2: development and validation of a coupled ecosystem-atmosphere model, scaling from surface fluxes of CO<sub>2</sub> and energy to atmospheric profiles." Geoscientific Model Development Discussions 6, no. 1 (2013): 1559–98. http://dx.doi.org/10.5194/gmdd-6-1559-2013.

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Abstract. The Weather Research &amp;amp; Forecasting meteorological (WRF) model has been coupled to the Soil Plant Atmosphere (SPA) terrestrial ecosystem model, to produce WRF-SPA. SPA generates realistic land-atmosphere exchanges through fully coupled hydrological, carbon and energy cycles. The addition of a land surface model (SPA) capable of modelling biospheric CO2 exchange allows WRF-SPA to be used for investigating the feedbacks between biosphere carbon balance, meteorology and land management/land use change. We have extensively validated WRF-SPA using multi-annual observations of air t
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Barr, Jordan G., Vic Engel, José D. Fuentes, et al. "Controls on mangrove forest-atmosphere carbon dioxide exchanges in western Everglades National Park." Journal of Geophysical Research: Biogeosciences 115, G2 (2010): n/a. http://dx.doi.org/10.1029/2009jg001186.

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Savage, K., T. R. Moore, and P. M. Crill. "Methane and carbon dioxide exchanges between the atmosphere and northern boreal forest soils." Journal of Geophysical Research: Atmospheres 102, no. D24 (1997): 29279–88. http://dx.doi.org/10.1029/97jd02233.

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Lamaux, E., A. Labatut, J. Fontan, A. Lopez, A. Druilhet, and Y. Brunet. "Biosphere atmosphere exchanges: Ozone and aerosol dry deposition velocities over a pine forest." Environmental Monitoring and Assessment 31-31, no. 1-2 (1994): 175–81. http://dx.doi.org/10.1007/bf00547194.

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Abril, Adriana B., Patricia A. Torres, and Enrique H. Bucher. "The importance of phyllosphere microbial populations in nitrogen cycling in the Chaco semi-arid woodland." Journal of Tropical Ecology 21, no. 1 (2005): 103–7. http://dx.doi.org/10.1017/s0266467404001981.

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In tropical rain forest, the interface between leaf surfaces and the atmosphere is a fundamental pathway for nutrient cycling (particulary nitrogen), possibly even more important than the soil–plant interface (Parker 1994, Silver et al. 1996). Most important nutrient exchanges in the phyllosphere–atmosphere interface are mediated by microbial populations. For example, some authors have considered that nitrogen fixation in the phyllosphere is the main mechanism for nitrogen gain in humid tropical ecosystems, because of the substantial nutrient demand resulting from a high plant productivity and
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Lamaud, E., Y. Brunet, A. Labatut, A. Lopez, J. Fontan, and A. Druilhet. "The Landes experiment: Biosphere-atmosphere exchanges of ozone and aerosol particles above a pine forest." Journal of Geophysical Research 99, no. D8 (1994): 16511. http://dx.doi.org/10.1029/94jd00668.

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Tesis sobre el tema "Forest-Atmosphere exchanges"

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Ahlm, Lars. "Aerosol exchange between forests and the atmosphere : fluxes over a tropical and a boreal forest /." Stockholm : Department of Applied Environmental Science (ITM), Stockholm University, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-38544.

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Diss. (sammanfattning) Stockholm : Stockholms universitet, 2010.<br>At the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 3: Submitted. Paper 4: manuscript. Härtill 5 uppsatser.
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Maurer, Kyle D. "Effects of Climate, Forest Structure, Soil Water, & Scale on Biosphere-Atmosphere Gas Exchange in a Great Lakes Mixed-Deciduous Forest." The Ohio State University, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=osu1366036482.

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Simon, Eric. "Modeling surface-atmosphere exchange of trace gases and energy within and above the Amazon rain forest." [S.l. : s.n.], 2004. http://deposit.ddb.de/cgi-bin/dokserv?idn=972311262.

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Alléon, Julien. "Vers une représentation à l'échelle globale du microclimat forestier dans le modèle de surfaces continentales ORCHIDEE." Electronic Thesis or Diss., université Paris-Saclay, 2024. http://www.theses.fr/2024UPASJ029.

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Les dynamiques temporelles et spatiales des échanges entre les surfaces continentales et l'atmosphère sont en grande partie contrôlées par la végétation. Dans un contexte de changement climatique, la précision de la modélisation des bilans d'énergie, d'eau et de dioxyde de carbone des écosystèmes dans les modèles de surfaces continentales revêt ainsi d'un double enjeu : elle permet d'améliorer la représentation des échanges entre les surfaces et l'atmosphère et, par conséquent, d'améliorer la fiabilité des modèles de climats ; et elle permet également de comprendre et de quantifier l'impact du
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Cambaliza, Maria Obiminda L. "Measurement of forest ecosystem-atmosphere exchange of 8¹³C-CO₂ using Fourier transform infrared spectroscopy and disjunct eddy covariance." Pullman, Wash. : Washington State University, 2010. http://www.dissertations.wsu.edu/Dissertations/Spring2010/m_cambaliza_121709.pdf.

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Thesis (Ph. D.)--Washington State University, May 2010.<br>Title from PDF title page (viewed on June 10, 2010). "Department of Civil and Environmental Engineering." Includes bibliographical references.
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Lindauer, Matthias [Verfasser], Hans Peter [Akademischer Betreuer] [Gutachter] Schmid, and Harald [Gutachter] Kunstmann. "Ecosystem-Atmosphere Exchange over a wind-throw-disturbed upland spruce forest in the Bavarian Forest National Park / Matthias Lindauer. Betreuer: Hans Peter Schmid. Gutachter: Harald Kunstmann ; Hans Peter Schmid." München : Universitätsbibliothek der TU München, 2016. http://d-nb.info/1104368285/34.

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Van, Delden Lona Petra Rike. "Implications of urbanization related land use change on the Carbon and Nitrogen cycle from subtropical soils." Thesis, Queensland University of Technology, 2017. https://eprints.qut.edu.au/109076/1/Lona_Van%20Delden_Thesis.pdf.

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This research established the first non-CO2 Global Warming Potential for subtropical peri-urban environments from the N2O and CH4 soil-atmosphere gas exchange dynamics after land use change due to urbanization. Two years of high temporal gas flux measurements identified immediate, seasonal and inter-annual C and N flux changes after turf grass establishment compared to forest and pasture land use to highlight the impact of our growing cities on the environment. Despite turf grass establishment increases soil greenhouse gas emissions, which increases the Global Warming Potential, the subtropica
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Hommeltenberg, Janina [Verfasser], Hans Peter [Akademischer Betreuer] Schmid, Matthias [Akademischer Betreuer] Drösler, Ralf [Akademischer Betreuer] Kiese, and Ankur [Akademischer Betreuer] Desai. "Biosphere-Atmosphere Exchange of CO2 and CH4 over Natural and Drained Bog Forest Ecosystems in Southern Germany / Janina Hommeltenberg. Gutachter: Matthias Drösler ; Ralf Kiese ; Ankur Desai ; Hans Peter Schmid. Betreuer: Hans Peter Schmid." München : Universitätsbibliothek der TU München, 2014. http://d-nb.info/106689714X/34.

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Geddes, Jeffrey. "Observations of Reactive Nitrogen Oxides: From Ground Level Ozone Production to Biosphere-atmosphere Exchange in Downwind Forest Environments." Thesis, 2013. http://hdl.handle.net/1807/35827.

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In urban areas, emissions of nitrogen oxide radicals (NOx ≡ NO + NO2) to the atmosphere from anthropogenic activities such as fossil fuel combustion contribute to poor air quality through the production of ozone and particulate matter. Soils are also a significant global source of NOx, but at downind forest environments the deposition of transported reactive nitrogen can be much more important than local emissions. Data from a government monitoring network in the Toronto area from 2000-2007 was used to explore the impact of long-term trends in NO2 and other ozone precursors on local ozone lev
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Simon, Eric [Verfasser]. "Modeling surface-atmosphere exchange of trace gases and energy within and above the Amazon rain forest / Eric Simon." 2004. http://d-nb.info/972311262/34.

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Libros sobre el tema "Forest-Atmosphere exchanges"

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Daytime turbulent exchange between the Amazon Forest and the atmosphere. Atmospheric Sciences Research Center, University at Albany, State University of New York, 1989.

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National Aeronautics and Space Administration (NASA) Staff. Daytime Turbulent Exchange Between the Amazon Forest and the Atmosphere. Independently Published, 2018.

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Capítulos de libros sobre el tema "Forest-Atmosphere exchanges"

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Monteny, B. A., J. M. Barbier, and C. M. Bernos. "Determination of the Energy Exchanges of a Forest-Type Culture: Hevea Brasiliensis." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_14.

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Jarvis, P. G., H. S. Miranda, and R. I. Muetzelfeldt. "Modelling Canopy Exchanges of Water Vapor and Carbon Dioxide in Coniferous Forest Plantations." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_31.

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Zhang, Zhenyu, Patrick Laux, Jussi Baade, Hassane Moutahir, and Harald Kunstmann. "Regional Land–Atmosphere Interactions in Southern Africa: Potential Impact and Sensitivity of Forest and Plantation Change." In Sustainability of Southern African Ecosystems under Global Change. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-10948-5_10.

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AbstractSouthern Africa is experiencing increasing land transformation and natural vegetation losses. Deforestation is one type of this land degradation where there are indigenous forests present, and afforestation of other nature ecosystems with timber plantations. This study performs regional coupled land–atmosphere model simulations using the Weather Research and Forecast (WRF) model with a resolution of 12 km, to assess the impact of forest and plantation cover change on regional climate in southern Africa. Three WRF simulations were designed for different land covers: (i) MODIS-derived la
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4

Lamaux, E., A. Labatut, J. Fontan, A. Lopez, A. Druilhet, and Y. Brunet. "Biosphere Atmosphere Exchanges: Ozone and Aerosol Dry Deposition Velocities Over a Pine Forest." In Non-CO2 Greenhouse Gases: Why and How to Control? Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-0982-6_18.

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Lewellen, W. S. "Modeling Turbulent Exchange in Forest Canopies." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_29.

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Hicks, B. B. "Application of Forest Canopy—Atmosphere Turbulent Exchange Information." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_37.

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Wesely, M. L., and R. L. Hart. "Variability of Short Term Eddy-Correlation Estimates of Mass Exchange." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_35.

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Desjardins, R. L., J. L. MacPherson, P. Alvo, and P. H. Schuepp. "Measurements of Turbulent Heat and CO2 Exchange Over Forests from Aircraft." In The Forest-Atmosphere Interaction. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5305-5_38.

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Dolman, A. J., E. J. Moors, T. Grunwald, P. Berbigier, and C. Bernhofer. "Factors Controlling Forest Atmosphere Exchange of Water, Energy, and Carbon." In Fluxes of Carbon, Water and Energy of European Forests. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05171-9_10.

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Duyzer, Jan, Hilbrand Weststrate, and Sam Walton. "Exchange of Ozone and Nitrogen Oxides Between the Atmosphere and Coniferous Forest." In Acid Reign ’95? Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-007-0864-8_32.

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Informes sobre el tema "Forest-Atmosphere exchanges"

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Danilo Dragoni, Hans Peter Schmid, C.S.B. Grimmond, J.C. Randolph, and J.R. White. Ecosystem-Atmosphere Exchange of Carbon, Water and Energy over a Mixed Deciduous Forest in the Midwest. Office of Scientific and Technical Information (OSTI), 2012. http://dx.doi.org/10.2172/1057580.

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Hollinger, David Y., Eric A. Davidson, Andrew D. Richardson, D. B. Dail, and N. Scott. Using model analyses and surface-atmosphere exchange measurements from the Howland AmeriFlux Site in Maine, USA, to improve understanding of forest ecosystem C cycling. Office of Scientific and Technical Information (OSTI), 2013. http://dx.doi.org/10.2172/1069294.

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