Tesi sul tema "Vegetation dynamics"
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Street, Lorna Elizabeth. "Carbon dynamics in Arctic vegetation". Thesis, University of Edinburgh, 2011. http://hdl.handle.net/1842/5651.
Testo completoSadler, Rohan. "Image-based modelling of pattern dynamics in a semiarid grassland of the Pilbara, Australia /". Connect to this title, 2006. http://theses.library.uwa.edu.au/adt-WU2007.0155.
Testo completoMcIntosh, Brian S. "Rule-based modelling of vegetation dynamics". Thesis, University of Edinburgh, 2002. http://hdl.handle.net/1842/12619.
Testo completoAnand, Madhur. "Towards a unifying theory of vegetation dynamics". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape16/PQDD_0002/NQ28471.pdf.
Testo completoGarcia-Carreras, Luis. "Atmospheric dynamics and convection over heterogeneous vegetation". Thesis, University of Leeds, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.535100.
Testo completoMandzy, Herring Luba T. "Vegetation dynamics and emvironmental change in Mongolia". Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.496582.
Testo completoPollock, Meg L. "Vegetation dynamics in seasonally grazed upland systems". Thesis, University of Edinburgh, 2003. http://hdl.handle.net/1842/856.
Testo completoCohen, Yoav. "A comparison between vegetation indices for measuring vegetation dynamics resulting from climate variations /". [Beer Sheva] : Ben Gurion University of the Negev, 2008. http://aranne5.lib.ad.bgu.ac.il/others/CohenYoav.pdf.
Testo completoCutler, Nick. "High-latitude vegetation dynamics : 850 years of vegetation development on Mt Hekla, Iceland". Thesis, University of Edinburgh, 2008. http://hdl.handle.net/1842/2485.
Testo completoArain, Muhammad Altaf. "Spatial aggregation of vegetation parameters in a coupled land surface-atmosphere model". Thesis, The University of Arizona, 1994. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_etd_hy0049_m_sip1_w.pdf&type=application/pdf.
Testo completoSavage, Shannon Lea. "Vegetation dynamics in Yellowstone's Northern Range 1985 - 1999 /". Thesis, Montana State University, 2005. http://etd.lib.montana.edu/etd/2005/savage/SavageS1205.pdf.
Testo completoThonicke, Kirsten. "Fire disturbance and vegetation dynamics analysis and models /". Phd thesis, [S.l. : s.n.], 2003. http://deposit.ddb.de/cgi-bin/dokserv?idn=968686885.
Testo completoDeng, Zhixin. "Vegetation dynamics in Oueme Basin, Benin, West Africa /". Göttingen : Cuvillier, 2007. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=016504013&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.
Testo completoAllchin, Elizabeth Ann. "Vegetation dynamics following management burning of lowland heathland". Thesis, University of Liverpool, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.284333.
Testo completoThureborn, Olle. "Dynamics in submersed Charophyta vegetation in three Swedish lakes". Thesis, Södertörns högskola, Institutionen för livsvetenskaper, 2011. http://urn.kb.se/resolve?urn=urn:nbn:se:sh:diva-15366.
Testo completoVegetationsdynamiken hos Charophytavegetation har studerats i tre grunda sjöar. De studerade sjöarna ligger ungefär 25 km sydost om Gävle, nära Östersjön. Sedimentproverna togs upp med hjälp av ett plaströr som fungerade som en sedimentprovtagare. Varje prov skivades sedan upp i tre skikt, undre, mellan och övre för att kunna studera vegetationsförändringar över tid. För de statistiska analyserna användes programmet R version 2.12.1 för windows. Syftet med denna studie var att beskriva hur vegetationsdynamiken förändras över tid i de tre utvalda sjöarna och utveckla metoder för att kunna använda sporbanken till dessa undersökningar. Totalt hittades tre arter i de studerade sjöarna, Chara intermedia, Chara aspera och Chara tomentosa. Resultaten visar att Chara generellt uppför sig olika mellan de olika samhällena, sjöarna har olika vegetationsdynamik. C. aspera och C. intermedia visade sig ha riktade förändringar medan C. tomentosa visade tydliga tecken på patch dynamik. Resultaten diskuteras utifrån olika tolkningar, som eutrofiering, salthaltsvariation , intraspecifik konkurrens och founder eller dominance- kontrollerade samhällen. Kransalger är känsliga för eutrofiering och många av de svenska arterna är idag rödlistade. Förståelsen för vegetationsdynamiken hos kransalgsarter är därför av stor relevans. Denna studie visar att det är möjligt att göra en undersökning av vegetationsdynamikens förändring över tid genom att använda sig av en sporbank.
Yang, Yongqian. "Impact of Patchy Vegetation on Wave and Runup Dynamics". Diss., Virginia Tech, 2016. http://hdl.handle.net/10919/72278.
Testo completoPh. D.
Ballantyne, Fiona. "Palaeoecology and vegetation dynamics in the Cederberg wilderness area". Master's thesis, University of Cape Town, 2010. http://hdl.handle.net/11427/6227.
Testo completoDavis, Jessica. "Soil seed bank dynamics in Mediterranean urban vegetation fragments". Thesis, Davis, Jessica (2012) Soil seed bank dynamics in Mediterranean urban vegetation fragments. Masters by Coursework thesis, Murdoch University, 2012. https://researchrepository.murdoch.edu.au/id/eprint/12926/.
Testo completoMcKune, Craig. "Rangeland condition in the Ceres Karoo: the importance of long-term studies". Bachelor's thesis, University of Cape Town, 2002. http://hdl.handle.net/11427/26017.
Testo completoRushworth, Garry. "Late Quaternary vegetation history of Craven, Yorkshire Dales". Thesis, University of Bradford, 2010. http://hdl.handle.net/10454/6286.
Testo completoOwen, Nia Wyn. "Plant ecology and community dynamics of machair systems in the Outer Hebrides". Thesis, University of Plymouth, 1998. http://hdl.handle.net/10026.1/780.
Testo completoGornall, Jemma. "The functional role of mosses in Arctic ecosystems". Thesis, University of Aberdeen, 2005. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=153316.
Testo completoRye, Timothy A. "Long-term functional trait dynamics in abandoned agricultural fields /". View online, 2008. http://repository.eiu.edu/theses/docs/32211131428174.pdf.
Testo completoWessollek, Christine, Babatunde Osunmadewa e Pierre Karrasch. "Introducing a rain-adjusted vegetation index (RAVI) for improvement of long-term trend analyses in vegetation dynamics". SPIE, 2015. https://tud.qucosa.de/id/qucosa%3A35057.
Testo completoOgunbadewa, Ebenezer Yemi. "Evaluating medium resolution satellite data for monitoring seasonal vegetation dynamics". Thesis, University of Salford, 2009. http://usir.salford.ac.uk/26845/.
Testo completoVasconcelos, Daniel. "Amphibian and Vegetation Dynamics in a Restored Wetland in Maine". Fogler Library, University of Maine, 2003. http://www.library.umaine.edu/theses/pdf/VasconcelosD2003.pdf.
Testo completoCorry, Patricia Mary Peet R. K. "Vegetation dynamics following grazing cessation on the Channel Islands, California". Chapel Hill, N.C. : University of North Carolina at Chapel Hill, 2006. http://dc.lib.unc.edu/u?/etd,160.
Testo completoTitle from electronic title page (viewed Oct. 10, 2007). "... in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Biology." Discipline: Biology; Department/School: Biology.
Sharp, Ben R. "Landscape-scale woody vegetation dynamics in an Australian tropical savanna". Thesis, University of Oxford, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.397462.
Testo completoClear, Jennifer. "Holocene fire and vegetation dynamics in the northern European forests". Thesis, University of Liverpool, 2013. http://livrepository.liverpool.ac.uk/16593/.
Testo completoGambin, Belinda. "Vegetation history and climate dynamics in Malta : a Holocene perspective". Thesis, Aix-Marseille, 2015. http://www.theses.fr/2015AIXM4384.
Testo completoThis thesis investigates the Holocene vegetation dynamics for Burmarrad in north-west Malta and provides a pollen-based quantitative palaeoclimatic reconstruction for this centrally located Mediterranean archipelago. The pollen record from this site provides new insight into the vegetation changes from 7280 to 1730 cal BP which correspond well with other regional records. The climate reconstruction for the area also provides strong correlation with southern (below 40oN) Mediterranean sites. The interpretation suggests an initially open landscape during the early Neolithic, surrounding a large palaeobay, developing into a dense Pistacia scrubland ca. 6700 cal BP. From about 4450 cal BP the landscape once again becomes open, coinciding with the start of the Bronze Age on the archipelago. This period is concurrent with increased climatic instability (between 4500 and 3700 cal BP) which is followed by a gradual decrease in summer moisture availability in the late Holocene. During the early Roman occupation period (1972 to 1730 cal BP) the landscape remains generally open with a moderate increase in Olea. This increase corresponds to archaeological evidence for olive oil production in the area, along with increases in cultivated crop taxa and associated ruderal species, as well as a rise in fire events. This thesis also provides a synthesis with the results from another core (BM1) taken from the same catchment area, as well as results of a preliminary modern surface pollen rain study. The Maltese archipelago provides important insight into vegetation, human impacts and climatic changes in an island context during the Holocene
Britton, Andrea Jane. "Modelling invasions on heathlands". Thesis, University of Liverpool, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.284563.
Testo completoSams, Brent Shipley. "Forest dynamics of pine- and oak-dominated communities on southeastern-facing slopes of Warm Springs Mountain, Virginia". Thesis, Virginia Tech, 2012. http://hdl.handle.net/10919/76803.
Testo completoMaster of Science
Fleming, Kelly M. "Functional diversity and life history traits of arbuscular mycorrhizal fungi in disturbed soils". Morgantown, W. Va. : [West Virginia University Libraries], 1999. http://etd.wvu.edu/templates/showETD.cfm?recnum=1191.
Testo completoTitle from document title page. Document formatted into pages; contains viii, 63 p. : ill. (some col.). Vita. Includes abstract. Includes bibliographical references.
Leppälä, M. (Mirva). "Successional changes in vegetation and carbon dynamics during boreal mire development". Doctoral thesis, Oulun yliopisto, 2011. http://urn.fi/urn:isbn:9789514294655.
Testo completoTiivistelmä Sukkessio on ekosysteemin lajistossa ja sen muissa ominaisuuksissa ajan kuluessa tapahtuva muutos. Suon kehitystä eli pitkäaikaista suosukkessiota vie eteenpäin turpeen paksuuskasvu, joka saa aikaan muutoksia suoekosysteemin hydrologiassa, kasvillisuudessa ja ravinnetilassa. Tästä johtuen myös suoekosysteemin erilaiset prosessit, kuten tuotanto sekä hajoamisen kautta tapahtuva hiilen vapautuminen eli hiilikaasutoiminta muuttuu suon ikääntyessä. Ekosysteemin hiilikaasutoiminnassa tapahtuvia muutoksia voidaan tutkia muun muassa mittaamalla ekosysteemin ja ilmakehän välisiä hiilidioksidi- ja metaanivirtoja. Boreaalisten luonnontilaisten soiden sukkessiota ja hiilidynamiikkaa on tutkittu runsaasti, mutta niiden välistä yhteyttä ei sen sijaan juuri tunneta. Tämän vuoksi ei tiedetä kuinka soiden hiilikaasutoiminta mahdollisesti muuttuu suon kehityksen aikana eli suosukkession edetessä. Tämän tutkimuksen päätavoitteena oli tutkia kuinka hiilidioksidin ja metaanin vaihdolla mitattu ekosysteemitoiminta muuttuu suon kehityksen aikana. Tutkimus pyrki myös selvittämään suosukkessiota kontrolloivat tekijät. Eri-ikäisten soiden hiilikaasudynamiikkaa tutkittiin mittaamalla hiilikaasuja Perämeren maankohoamisrannikolla kahdeksan kilometrin pituisella sukkessiogradientilla, joka koostuu primaarisoistumisen kautta syntyneistä soista. Soiden lyhyestä keskinäisestä etäisyydestä johtuen ne ovat olleet saman ilmastollisen kontrollin alaisena suurimman osan kehityksestään. Vaiheittainen kasvilajien muutos sukkessiogradientilla yhdessä kasvilajien erilaisen yhteyttämispotentiaalin, fenologian ja yhteyttävän lehtipinta-alan kanssa johti hiilidioksidivaihdon alhaisempaan tasoon sekä pienempään ajalliseen vaihteluun vanhemmilla sukkessiovaiheilla. Myös metaanin vaihdolla oli alhaisimmat vuosien väliset vaihtelut vanhemmilla vaiheilla. Yleisesti ottaen metaanipäästöt kasvoivat suon iän myötä, vaikkakaan tätä trendiä ei havaittu sateisena kasvukautena. Lisäksi tutkimus osoitti, että talviaikaiset hiilivirrat (CO2, CH4) seurasivat kesäaikaisen hiilidynamiikan vaihtelua. Kasvillisuuden keskeinen rooli ekosysteemin sukkessiossa havaittiin myös tässä tutkimuksessa. Kasvillisuuden ohella merkittäväksi suosukkessiota sääteleväksi tekijäksi osoittautui hydrologisten olojen vaikutus. Tasaisemmat hydrologiset olot vanhemmilla sukkessiovaiheilla johtivat vähäisempään ajalliseen vaihteluun metaani- ja hiilidioksidivirroissa. Tutkimuksen tulokset viittaavat siihen, että ekosysteemin hiilidynamiikka stabilisoituu suon kehityksen aikana lisääntyvän autogeenisen kontrollin kautta
Propastin, Pavel. "Remote sensing based study on vegetation dynamics in drylands of Kazakhstan". Doctoral thesis, Stuttgart Ibidem-Verl, 2007. http://hdl.handle.net/11858/00-1735-0000-0006-B26A-A.
Testo completoTzedakis, Polychronis Constantinos. "Vegetation dynamics in northwest Greece in response to Quaternary climatic cycles". Thesis, University of Cambridge, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239164.
Testo completoWang, Guiling 1971. "The role of vegetation dynamics in the climate of West Africa". Thesis, Massachusetts Institute of Technology, 2000. http://hdl.handle.net/1721.1/17486.
Testo completoIncludes bibliographical references (p. 211-224).
The climate of West Africa exhibits significant variability at the time scale of decades. The persistent drought of the past three decades is an example of such variability. This study investigates the role of vegetation dynamics in shaping the low-frequency variability of the climate over West Africa. A zonally symmetric, synchronously coupled biosphere-atmosphere model (ZonalBAM) which includes explicit representation of vegetation dynamics has been developed, and has been validated using observations on both the atmospheric and biospheric climate. The model is then used to study the dynamics of the coupled biosphere-atmosphere system over West Africa. Based on the model sensitivity to initial conditions and the resilience of the coupled system with respect to perturbations, we demonstrate that the coupled biosphere-atmosphere system over West Africa has multiple equilibrium states, with reversible transitions between different equilibria. The two-way biosphere-atmosphere feedback is a significant process in both climate persistence and climate transition. Based on long-term climate simulations using ZonalBAM driven with the observed sea surface temperature (SST) variations, our study shows that vegetation dynamics is a significant process in shaping the climate variability of West Africa. The response of the regional climate system to large-scale forcings is significantly regulated by vegetation dynamics. The relatively slow response of vegetation to changes in the atmosphere is a significant mechanism that acts to enhance the low-frequency rainfall variability. Climate transitions between different equilibria act as another mechanism contributing to the low-frequency rainfall variability - multi-decadal fluctuations can take place as a collective reflection of climate persistence at one equilibrium and climate transition towards another. Vegetation dynamics seems to play an important role in the development and persistence of the current Sahel drought. The most likely scenario for the triggering mechanism of the Sahel drought would involve a combination of several processes including regional changes in land cover as well as changes in the patterns of global and regional SST distributions. However, regardless of the nature of the triggering mechanism, the response of the natural vegetation to the atmospheric changes is the critical process in the development and persistence of the observed drought.
by Guiling Wang.
Ph.D.
Marchant, Robert. "Late Quarternary montane vegetation dynamics in Bwindi-impenetrable forest, Central Africa". Thesis, University of Hull, 1997. http://hydra.hull.ac.uk/resources/hull:11561.
Testo completoWania, Rita. "Modelling northern peatland land surface processes, vegetation dynamics and methane emissions". Thesis, University of Bristol, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.685934.
Testo completoBórnez, Mejías Kevin. "Study of vegetation dynamics from satellite: phenological responses to climate change". Doctoral thesis, Universitat Autònoma de Barcelona, 2021. http://hdl.handle.net/10803/673693.
Testo completoLa fenología es clave para controlar los procesos fisicoquímicos y biológicos, especialmente el albedo, la rugosidad superficial, conductancia de las hojas, flujos de carbono, agua y energía. Por lo tanto, la estimación de la fenología es cada vez más importante para comprender los efectos del cambio climático en los ecosistemas y las interacciones biosfera-atmósfera. La teledetección es una herramienta útil para caracterizar la fenología, aunque no existe consenso sobre el tipo de sensor satelital y metodología óptimos para extraer métricas fenológicas. Los objetivos principales de mi investigación fueron (i) mejorar la estimación de la fenología vegetal a partir de datos satelitales, (ii) validar las estimaciones fenológicas con observaciones terrestres y teledetección cercana a la superficie, y (iii) comprender las relaciones entre las variables climáticas y la fenología en un contexto de cambio climático, así como evaluar las respuestas de la vegetación a eventos extremos. Estos objetivos se exploran en los siguientes tres capítulos de la tesis. En el capítulo 2, investigué la sensibilidad de la fenología a (I) la variable de vegetación: índice de vegetación NDVI, índice de área foliar (LAI), fracción de radiación fotosintéticamente activa absorbida (FAPAR) y fracción de cubierta vegetal (FCOVER); (II) el método de suavizado para derivar trayectorias estacionales; y (III) el método de estimación fenológica: umbrales, función logística, media móvil y primera derivada. El método basado en umbrales aplicado a la serie temporal Copernicus Global Land LAI V2 suavizada dio resultados óptimos al validarlos con observaciones terrestres, con errores cuadráticos medios de ~10 d y ~25 d para el inicio de estación fenológica y la senescencia respectivamente. En el tercer capítulo, utilicé medidas fenológicas continuas de PhenoCam y FLUXNET a alta resolución temporal (30 minutos). Esto permite una comparación más robusta y precisa con la fenología estimada a partir de satélite, evitando problemas relacionados con las diferencias en la definición de métricas fenológicas. Validé la fenología estimada a partir de series de tiempo de LAI con PhenoCam y FluxNet en 80 bosques caducifolios. Los resultados mostraron una fuerte correlación (R2 > 0,7) entre la fenología obtenida mediante teledetección y las observaciones terrestres para el inicio de estación y R2 > 0,5 para el final de estación. El método basado en umbrales funcionó mejor con un error cuadrático medio de ~9 d con PhenoCam y ~7 d con FLUXNET para el inicio de estación, y ~12 d y ~10 d, respectivamente, para la senescencia. En el cuarto capítulo, investigué los patrones espacio-temporales de la respuesta fenológica a las anomalías climáticas en el hemisferio norte utilizando la fenología estimada en el Capítulo 2 y validado en el Capítulo 2 y Capítulo 3, y conjuntos de datos climáticos de múltiples fuentes para 2000-2018 a resoluciones de 0.1°. También evalué el impacto de las olas de calor extremas y las sequías en la fenología. Los análisis de correlación parcial de las métricas fenológicas estimadas con satélite y las variables climáticas, indicaron que los cambios en la temperatura pre estacional tuvieron mayor influencia sobre las anomalías fenológicas que la precipitación: cuanto mayor es la temperatura, más temprano es el comienzo estacional en la mayoría de los bosques caducifolios (coeficiente de correlación medio de -0,31). Tanto la temperatura como la precipitación contribuyeron al avance y retraso del final de estación. Un atraso en la senescencia se correlacionó significativamente con un índice de precipitación-evapotranspiración estandarizado (SPEI) positivo (~ 30% de los bosques). El final e inicio de estación cambió >20 d en respuesta a la ola de calor en la mayor parte de Europa en 2003 y en los Estados Unidos de América en 2012.
Phenology is key to control physicochemical and biological processes, especially albedo, surface roughness, canopy conductance and fluxes of carbon, water and energy. High-quality retrieval of land surface phenology (LSP) is thus increasingly important for understanding the effects of climate change on ecosystem function and biosphere–atmosphere interactions. Remote sensing is a useful tool for characterizing LSP although no consensus exists on the optimal satellite dataset and the method to extract phenology metrics. I aimed to (i) improve the retrieval of Land Surface Phenology from satellite data, (ii) validate LSP with ground observations and near surface remote sensing, and (iii) understand the relationships between climate variables and phenology in a climate change context, as well as to assess the responses of vegetation to extreme events. These three main research objectives are explored in the three chapters of the thesis. In chapter 2, I investigated the sensitivity of phenology to (I) the input vegetation variable: normalized difference vegetation index (NDVI), leaf area index (LAI), fraction of absorbed photosynthetically active radiation (FAPAR), and fraction of vegetation cover (FCOVER); (II) the smoothing and gap filling method for deriving seasonal trajectories; and (III) the phenological extraction method: threshold, logistic-function, moving-average and first derivative based approaches. The threshold-based method applied to the smoothed and gap-filled Copernicus Global Land LAI V2 time series agreed the best with the ground phenology, with root mean square errors of ~10 d and ~25 d for the timing of the start of the season (SoS) and the end of the season (EoS), respectively. In the third chapter, I took advantage of PhenoCam and FLUXNET capability of continuous monitoring of vegetation seasonal growth at very high temporal resolution (every 30 minutes). This allows a more robust and accurate comparison with LSP derived from satellite time series avoiding problems related to the differences in the definition of phenology metrics. I validated LSP estimated from LAI time series with near-surface PhenoCam and eddy covariance FLUXNET data over 80 sites of deciduous broadleaf forest. Results showed a strong correlation (R2 > 0.7) between the satellite LSP and ground-based observations from both PhenoCam and FLUXNET for the timing of the start (SoS) and R2 > 0.5 for the end of season (EoS). The threshold-based method performed the best with a root mean square error of ~9 d with PhenoCam and ~7 d with FLUXNET for the timing of SoS, and ~12 d and ~10 d, respectively, for the timing of EoS. In the fourth chapter, I investigated the spatio-temporal patterns of the response of deciduous forests to climatic anomalies in the Northern Hemisphere using LSP derived in Chapter 1 and validated in Chapter 1 and Chapter 2, and multi-source climatic data sets for 2000–2018 at resolutions of 0.1°. I also assessed the impact of extreme heatwaves and droughts on deciduous forest phenology. Analyses of partial correlations of phenological metrics with the timing of the start of the season (SoS), end of the season (EoS), and climatic variables indicated that changes in preseason temperature played a stronger role than precipitation in the interannual variability of SoS anomalies: the higher the temperature, the earlier the SoS in most deciduous forests in the Northern Hemisphere (mean correlation coefficient of -0.31). Both temperature and precipitation contributed to the advance and delay of EoS. A later EoS was significantly correlated with a positive standardized precipitation-evapotranspiration index (SPEI) at the regional scale (~30% of deciduous forests). The timings of EoS and SoS shifted by >20 d in response to heat waves throughout most of Europe in 2003 and in the United States of America in 2012.
Universitat Autònoma de Barcelona. Programa de Doctorat en Ecologia Terrestre
Wang, Haitao. "Monitoring vegetation dynamics in Zhongwei, an arid city of Northwest China". Thesis, Virginia Tech, 2014. http://hdl.handle.net/10919/48893.
Testo completoMaster of Science
González, Jaramillo Víctor Hugo [Verfasser], e Jörg [Akademischer Betreuer] Bendix. "Vegetation Dynamics in Ecuador / Víctor Hugo González-Jaramillo ; Betreuer: Jörg Bendix". Marburg : Philipps-Universität Marburg, 2020. http://d-nb.info/1205069143/34.
Testo completoOgutu, Zadoc A. "Human disturbances and vegetation dynamics in the Narok district of Kenya". Thesis, University of Edinburgh, 1991. http://hdl.handle.net/1842/20072.
Testo completoRoot, Brian G. "Alkaline wetland vegetation dynamics at North Dakota piping plover nesting beaches /". free to MU campus, to others for purchase, 1996. http://wwwlib.umi.com/cr/mo/fullcit?p9737863.
Testo completoHerbert, Rachel Rosemarie. "Vegetation and nutrient dynamics of forested riparian wetlands in agricultural settings". College Park, Md. : University of Maryland, 2005. http://hdl.handle.net/1903/2547.
Testo completoThesis research directed by: Marine, Estuarine, Environmental Sciences Graduate Program . Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
Kellerman, Millicent Johanna Susanna. "Seed bank dynamics of selected vegetation types in Maputaland, South Africa". Diss., Connect to this title online, 2004. http://upetd.up.ac.za/thesis/available/etd-02012005-090837.
Testo completoGonzález-Jaramillo, Víctor Hugo [Verfasser], e Jörg [Akademischer Betreuer] Bendix. "Vegetation Dynamics in Ecuador / Víctor Hugo González-Jaramillo ; Betreuer: Jörg Bendix". Marburg : Philipps-Universität Marburg, 2020. http://d-nb.info/1205069143/34.
Testo completovon, Behren Christa. "Composition and Dispersal Dynamics of Vegetation Communities in Urban Riparian Forests". PDXScholar, 2018. https://pdxscholar.library.pdx.edu/open_access_etds/4409.
Testo completoKim, Su Jin. "3D numerical simulation of turbulent open-channel flow through vegetation". Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/42892.
Testo completoFang, Yiman. "Relationships between surface pollen and vegetation in the Meiling Mountains, southeast China : an aid to reconstruct past vegetation dynamics". Thesis, University of Hull, 2018. http://hydra.hull.ac.uk/resources/hull:17103.
Testo completo