How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.

the Biotic Pump Theory, as set forward by Drs. Makarieva and Gorshkov, states that the primary force driving surface winds, certainly in the tropics, is induced by the negative changes in atmospheric pressure caused by condensation of water vapour when clouds form. A high rate of condensation is nec...

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Autores:: Bunyard, Peter

Tipo de recurso:: Book

Fecha de publicación:: 2014

Institución:: Universidad Sergio Arboleda

Repositorio:: Repositorio U. Sergio Arboleda

Idioma:: eng

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dc.title.eng.fl_str_mv	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
title	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
spellingShingle	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?. Climatología Circulación atmosférica Ciclo hidrológico Teoría de la bomba biótica Climatology Atmospheric circulation Hydrologic cycle OTHER Biotic pump theory
title_short	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
title_full	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
title_fullStr	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
title_full_unstemmed	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
title_sort	How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.
dc.creator.fl_str_mv	Bunyard, Peter
dc.contributor.author.spa.fl_str_mv	Bunyard, Peter
dc.subject.lemb.spa.fl_str_mv	Climatología Circulación atmosférica Ciclo hidrológico Teoría de la bomba biótica
topic	Climatología Circulación atmosférica Ciclo hidrológico Teoría de la bomba biótica Climatology Atmospheric circulation Hydrologic cycle OTHER Biotic pump theory
dc.subject.lemb.eng.fl_str_mv	Climatology Atmospheric circulation Hydrologic cycle OTHER Biotic pump theory
description	the Biotic Pump Theory, as set forward by Drs. Makarieva and Gorshkov, states that the primary force driving surface winds, certainly in the tropics, is induced by the negative changes in atmospheric pressure caused by condensation of water vapour when clouds form. A high rate of condensation is necessary and therefore the theory requires that a suffciently high rate of evapotranspiration from large areas of forest provides the "fuel" for the process. The theory therefore runs contrary to the traditional view, as introduced in climate models, that surface winds are the sole products of differences in surface heating as well as of latent heat release during the process of condensation. Indeed, Makarieva and her colleagues claim that transitions in the phases of water play a far more important role in driving atmospheric dynamics than is currently recognised
publishDate	2014
dc.date.created.spa.fl_str_mv	2014
dc.date.issued.spa.fl_str_mv	2014-02
dc.date.accessioned.spa.fl_str_mv	2015-08-21T18:53:51Z 2016-05-11T14:38:11Z 2017-05-16T19:01:51Z
dc.date.available.spa.fl_str_mv	2015-08-21T18:53:51Z 2016-05-11T14:38:11Z 2017-05-16T19:01:51Z
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dc.type.local.spa.fl_str_mv	Libro completo
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dc.identifier.isbn.spa.fl_str_mv	978-958-8745-89-3
dc.identifier.uri.eng.fl_str_mv	http://hdl.handle.net/11232/397
dc.identifier.doi.eng.fl_str_mv	https://doi.org/10.22518/9789588745886
dc.identifier.instname.spa.fl_str_mv	instname:Universidad Sergio Arboleda
dc.identifier.reponame.spa.fl_str_mv	reponame:Repositorio Institucional Universidad Sergio Arboleda
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identifier_str_mv	978-958-8745-89-3 instname:Universidad Sergio Arboleda reponame:Repositorio Institucional Universidad Sergio Arboleda repourl:https://repository.usergioarboleda.edu.co/
url	http://hdl.handle.net/11232/397 https://doi.org/10.22518/9789588745886
dc.language.iso.eng.fl_str_mv	eng
language	eng
dc.relation.ispartofseries.spa.fl_str_mv	Investigación
dc.relation.references.spa.fl_str_mv	Avissar, R., & Werth, D. (2005). Global Hydroclimatological Teleconnections Resulting from Tropical Deforestation. Journal of Hydrometeorology, 6(2), 134-145. doi: 10.1175/JHM406.1 Bunyard, P. (2014). How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?. Bogotá : Universidad Sergio Arboleda Betts, R. A., Sanderson, M., & Woodward, S. (2008). Effects of large-scale Amazon forest degradation on climate and air quality through fluxes of carbon dioxide, water, energy, mineral dust and isoprene. Philosophical Transactions of the Royal Society B, 363(1498), 1873-1880. doi: 10.1098/rstb.2007.0027 Betts, R. A., Cox, P.M., Collins, M., Gash, J.H., Harris, P.P., Huntingford, C., Jones, C.D., et al. (2002). Amazonian forest die-backin the Hadley Centre coupled climate-vegetation model. Exeter, UK: UK Met Office, Hadley Centre. Blyth, E., Gash, J., Lloyd, A., Pryor M., Weedon, G. P., & Shuttleworth, J. (2010). Evaluating the JULES Land Surface Model Energy Fluxes Using FLUXNET Data. Journal of Hydrometeorology, 11, 509-519. doi:10.1175/2009JHM1183.1 Boyce, C. K., Brodribb, T. J., Feild, T. S., & Zwieniecki, M. A. (2009). Angiosperm leaf vein evolution was physiologically and environmentally transformative. Proceedings of The Royal Society B, 276(1663), 1771-1776. doi: 10.1098/rspb.2008.1919 Boyce, C. K., & Lee, J. E. (2010). An exceptional role for flowering plant physiology in the expansion of tropical rainforests and biodiversity. Proceedings of Royal Society B, 277, 3437-3443. doi: 10.1098/rspb.2010.0485 Boyce, C. K., Lee, J. E., Feild, T. S., Brodribb, T. J., & Zwieniecki, M. A. (2010). Angiosperms helped put the rain in the rainforests: the impact of plant physiological evolution on tropical biodiversity. Annals of the Missouri Botanical Garden, 97(4), 527-540. doi: 10.3417/2009143 Brubaker, K. L, Dara E., & Eagleston, P. S. (1993). Estimation of Continental Precipitation Recycling. Journal of Climate, 6(6), 1077-1089. doi: 10.1175/15200442(1993)006<1077:EOCPR>2.0.CO;2 Bunyard, P. (2011). ¿Es aleatorio que la tierra ha retenido su agua?. Recovery from http:// www.almamater.edu.co / sitio / Archivos / Documentos /Documentos/00000534.pdf Bunyard, P. (2012). Biotic Pump, Fiction or Reality?. Awaiting publication. Bunyard, P., Netchev, P., Peña, C., & Redondo, J. (2012). The Barometric tidal wave, what is it?. Work presented at Tunis. Butler, R. (2010). The Amazongate fiasco. Recovery from http://news.mongabay.com/2010/0204-amazongate.html Charney, J., Quirk, W., Chow, S., & Kornfield, J. (1977). A comparative study of the effects of albedo change on drought in semiarid regions. Journal of Atmospheric Sciences, 34, 1366-1385. doi:10.1175/15200469(1977)034<1366:ACSOTE>2.0.CO;2 Collatz, G. J., Ribas-Carbfdbo, M. & Berry, J. A. (1992). Coupled Photosynthesis- Stomatal conductance model for Australian Journal of Plant Physiology, 19(5), 519-538. Cox, P. M., Betts, R. A., Jones, C. D., Spall, S. A., & Totterdell, I. J. (2000). Acceleration of global-warming due to carbon-cycle feedbacks in a coupled climate model. Nature, 408, 184-187. doi: 10.1038/35041539 Cox, P. M., Huntingford, C., & Harding, R. J., (1998). A canopy conductance and photosynthesis model for use in a GCM land surface scheme. Journal of Hydrology, 212- 213, 79-94. doi: 10.1016/S0022-1694(98)00203-0 Cowling, S. A., Maslin, M. A., & Sykes, M. T. (2001). Paleovegetation Simulations of Lowland Amazonia and Implications for Neotropical Allopatry and Speciation. Quaternary Research, 55(2), 140-149. doi: 10.1006/qres.2000.2197 Cowling, S. A., Shin, Y., Pinto, E., & Jones C. D. (2008). Water recycling by Amazonian vegetation: coupled versus uncoupled vegetation–climate interactions. Philosophical Transactions of The Royal Society B, 363(1498), 1865-1871. 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Assessing the role of deep rooted vegetation in the climate system with model simulations: mechanism, comparison to observations and implications for Amazonian deforestation. Climate Dynamics, 16(2-3), 183-199. Kleidon, A. (2002). Testing the Effect of Life on Earth’s Functioning: How Gaian Is the Earth System? Climatic Change, 52(4), 383-389. doi: 10.1023/A:1014213811518 Kleidon, A. (2004). Amazonian Biogeography as a Test for Gaia. In S. Schneider, J. Miller, E. Crist, & P. Boston (Eds.), Scientists Debate Gaia: The Next Century (pp. 289-291). Oxford: MIT Press Scholarship Online. doi:10.7551/mitpress/9780262194983.003.0027 Kleidon, A. (2004). Amazonian Biogeography as a Test for Gaia. In S. Schneider, J. Miller, E. Crist, & P. Boston (Eds.), Scientists Debate Gaia: The Next Century (pp. 289-291). Oxford: MIT Press Scholarship Online. doi:10.7551/mitpress/9780262194983.003.0027 Makarieva, A. M., & Gorshkov, V. G. (2007). Biotic pump of atmospheric moisture as driver of the hydrological cycle on land. Hydrology and Earth System Sciences, 11, 1013-1033. doi:10.5194/hess-11-1013-2007 Makarieva, A. M., & Gorshkov, V. G. (2009a). Condensation-induced dynamic gas fluxes in a mixture of condensable and non-condensable gases. Physics Letters A, 373(32), 2801-2804. doi:10.1016/j.physleta.2009.05.057 Makarieva, A. M., & Gorshkov, V. G. (2009b). Condensation-induced kinematics and dynamics of cyclones, hurricanes and tornadoes. Physics Letters A, 373(46), 4201-4205. doi: 10.1016/j.physleta.2009.09.023 Makarieva, A. M., & Gorshkov, V. G. (2009c). Reply to A. G. C. A. Meesters et al.’s comment on “Biotic pump of atmospheric moisture as driver of the hydrological cycle on land. Hydrology and Earth System Sciences, 13(17), 1307–1311. doi: 10.5194/hess-13-1307-2009 Makarieva, A. M., & Gorshkov, V. G. (2010). Potential energy of atmospheric water vapor and the air motions induced by water vapor condensation on different spatial scales. Biotic Regulation. Recovery fromarXiv:1003.5466v1 . Makarieva, A. M., Gorshkov, V. G., & Li, B. (2006). Conservation of water cycle on land via restoration of closed-canopy forests: implications for regional landscape planning. Ecological Research, 21(6), 897-906. doi:10.1007/s11284-006-0036-6 Makarieva, A. M., Gorshkov, V. G., & Li, B. L. (2013). Revisiting forest impact on atmospheric water vapor transport and precipitation. Theoretical and Applied Climatology, 111(1-2), 79-96. doi: 10.1007/s00704-012-0643-9 Marengo, J. A. (2004). Interdecadal and long term rainfall variability in the Amazon basin. Theoretical and Applied Climatology, 78(1-3), 79-96. doi:10.1007/s00704-004-0045-8 Marengo, J. A. (2006). On the hydrological cycle of the Amazon basin: A historical review and current state-of-the-art. Revista Brasileira de Meteorologia, 21(3), 1-19. Marengo, J. A. (2006). On the hydrological cycle of the Amazon basin: A historical review and current state-of-the-art. Revista Brasileira de Meteorologia, 21(3), 1-19. Marengo, J. A., Nobre, C.A., Tomasella, J., Cardoso, M.F, & Oyama, M.D. (2008). Hydro-climatic and ecological behaviour of the drought of Amazonia in 2005. Philosophical Transactions of The Royal Society B Biological Sciences, 363(1498), 1773-1778. doi: 10.1098/rstb.2007.0015 Maslin, A. M., Ettwein, V. J., Boot, C. S., Bendle, J., & Pancost, R. D. (2012). Amazon Fan biomarker evidence against the Pleistocene rainforest refuge hypothesis? Journal of Quaternary Science, 27 (5), 451-460. doi: 10.1002/jqs.1567. Meteorological Office (s.f.). Meteorological data from 1961 to 2011 of Finland. Molion, L. C. (1989). The Amazonian Forests and Climatic Stability Impact of deforestation on Amazonia. The Ecologist, 19(6), 207-210. Morton, D. C., Nagol, J., Carabajal, C. C., Rosette, J., Palace, M., Cook, B. D., Vermote, E. 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spelling	Atribución-NoComercial-SinDerivadas 2.5 Colombia (CC BY-NC-ND 2.5 CO)http://repository.usergioarboleda.edu.co/bitstream/id/5bccc72d-7e6d-4f64-ab18-bad93c49a567/license.txthttp://creativecommons.org/licenses/by-nc-nd/2.5/co/Abierto (Texto Completo)http://purl.org/coar/access_right/c_abf2Bunyard, Peter2015-08-21T18:53:51Z2016-05-11T14:38:11Z2017-05-16T19:01:51Z2015-08-21T18:53:51Z2016-05-11T14:38:11Z2017-05-16T19:01:51Z20142014-02978-958-8745-89-3http://hdl.handle.net/11232/397https://doi.org/10.22518/9789588745886instname:Universidad Sergio Arboledareponame:Repositorio Institucional Universidad Sergio Arboledarepourl:https://repository.usergioarboleda.edu.co/the Biotic Pump Theory, as set forward by Drs. Makarieva and Gorshkov, states that the primary force driving surface winds, certainly in the tropics, is induced by the negative changes in atmospheric pressure caused by condensation of water vapour when clouds form. A high rate of condensation is necessary and therefore the theory requires that a suffciently high rate of evapotranspiration from large areas of forest provides the "fuel" for the process. The theory therefore runs contrary to the traditional view, as introduced in climate models, that surface winds are the sole products of differences in surface heating as well as of latent heat release during the process of condensation. Indeed, Makarieva and her colleagues claim that transitions in the phases of water play a far more important role in driving atmospheric dynamics than is currently recognisedLa teoría de la bomba biótica , establece que la primera fuerza motriz de los vientos de superficie, sobre todo en los trópicos , es inducida por los cambios negativos en la presión atmosférica causada por la condensación de vapor de agua cuando las nubes se forman. Una alta velocidad de condensación es necesaria y por lo tanto, la teoría requiere que una alta evapotranspiración de grandes áreas de bosques que proporcionan el "combustible" para el proceso. Por consiguiente, la teoría va en contra de la visión tradicional , como se presentó en los modelos climáticos , que los vientos de superficie son los únicos productos de diferencias de calentamiento de la superficie, así como de la liberación del calor latente durante el proceso de condensación. De hecho , Makarieva y sus colegas afirman que las transiciones en las fases de agua juegan un papel más importante en el impulso de la dinámica atmosférica de lo que se reconoce actualmente.114Digitalapplication/pdfengUniversidad Sergio ArboledaInstituto de Estudios y Servicios Ambientales - IDEASAInvestigaciónAvissar, R., & Werth, D. (2005). Global Hydroclimatological Teleconnections Resulting from Tropical Deforestation. Journal of Hydrometeorology, 6(2), 134-145. doi: 10.1175/JHM406.1Bunyard, P. 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Journal of Climatology, 3(3), 337-352. doi:10.1175/15200442(1990)003<0337:IOBFOT>2.0.CO;23114How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.ClimatologíaCirculación atmosféricaCiclo hidrológicoTeoría de la bomba bióticaClimatologyAtmospheric circulationHydrologic cycleOTHER Biotic pump theoryhttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_2f33http://purl.org/redcol/resource_type/LIBLibro completoLICENSElicense.txttext/plain1161https://repository.usergioarboleda.edu.co/bitstream/11232/397/1/license.txt97a964ad860602f11de1a47e333f3c18MD51open accessTHUMBNAILHow the biotic pump.pdf.jpgHow the biotic pump.pdf.jpgGenerated Thumbnailimage/jpeg7282https://repository.usergioarboleda.edu.co/bitstream/11232/397/6/How%20the%20biotic%20pump.pdf.jpgeb7f8d9b741e4f438e4d11bd00ca5f53MD56open accessTEXTHow the biotic pump.pdf.txtHow the biotic pump.pdf.txtExtracted texttext/plain193196https://repository.usergioarboleda.edu.co/bitstream/11232/397/4/How%20the%20biotic%20pump.pdf.txtff865702090d338554582be80afea54bMD54open accessORIGINALHow the biotic pump.pdfHow the biotic pump.pdfLibroapplication/pdf5340693https://repository.usergioarboleda.edu.co/bitstream/11232/397/7/How%20the%20biotic%20pump.pdf4aae9d4256d17191be8c36edceeff0a6MD57open access11232/397oai:repository.usergioarboleda.edu.co:11232/3972022-11-22 17:32:49.518open accessRepositorio Institucional Universidad Sergio Arboledadspace-help@myu.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

How the Biotic Pump links the hydrological and the rainforest to climate : ¿Is it for real? ¿How can we prove it?.

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