Academic literature on the topic 'Dendroecology'

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Journal articles on the topic "Dendroecology"

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Bräuning, Achim. "Dendroecology in Asia." Trees 27, no. 2 (February 26, 2013): 341–42. http://dx.doi.org/10.1007/s00468-013-0862-4.

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Allen, K. "Dendroecology: principles and practice." Australian Forestry 83, no. 2 (April 2, 2020): 99–100. http://dx.doi.org/10.1080/00049158.2020.1771649.

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Manzanedo, Rubén D. "Dendroecology: Principles and Practice." Tree-Ring Research 76, no. 2 (August 31, 2020): 102. http://dx.doi.org/10.3959/trr2020-9.

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Schmid, Rudolf, and Fritz Hans Schweingruber. "Tree Rings and Environment: Dendroecology." Taxon 46, no. 3 (August 1997): 604. http://dx.doi.org/10.2307/1224418.

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Manzanedo, Rubén D., and Neil Pederson. "TOWARDS A MORE ECOLOGICAL DENDROECOLOGY." Tree-Ring Research 75, no. 2 (August 7, 2019): 152. http://dx.doi.org/10.3959/1536-1098-75.2.152.

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Rauchfuss, Julia. "Autobox and its use in Dendroecology." Tree-Ring Research 67, no. 1 (January 2011): 63–64. http://dx.doi.org/10.3959/2010-8.1.

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Rozendaal, Danaë M. A., and Pieter A. Zuidema. "Dendroecology in the tropics: a review." Trees 25, no. 1 (August 31, 2010): 3–16. http://dx.doi.org/10.1007/s00468-010-0480-3.

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Misson, Laurent. "MAIDEN: a model for analyzing ecosystem processes in dendroecology." Canadian Journal of Forest Research 34, no. 4 (April 1, 2004): 874–87. http://dx.doi.org/10.1139/x03-252.

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Ecophysiological and dendroecological data from a temperate sessile oak (Quercus petraea (Matt.) Liebl.) stand in Belgium were used to develop and parameterize a dendroecological process-based model. The purpose of this model is to serve as a tool for exploring the relationship between climate variability and tree growth based on dendro ecological data. When parameterized, the model was able to correctly simulate measurements of bud-burst date, through fall (r2 = 0.95), soil water content (r2 = 0.81), transpiration (r2 = 0.80), and ring-width series from 1960 to 1999 (r2 = 0.46). Model sensitivity analysis showed that atmospheric vapor pressure deficit is the major controlling factor of transpiration in this type of ecosystem. The model shows that bole increment is principally controlled by temperature because it affects the phenological process of bud burst and thus the growing season length. Precipitation variability does not affect variation of transpiration rate and bole increment because calculated soil water stress is negligible during the simulation period. Discrepancies between observed and simulated bole increment may be a consequence of stand density variations and worm defoliation in the spring. The MAIDEN model is particularly suited for dendreocological analysis because it takes simple species, site condition, and climatic variables as input.
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Bräuning, Achim. "Editorial note for the special issue on ‘Tropical Dendroecology’." Trees 25, no. 1 (December 24, 2010): 1–2. http://dx.doi.org/10.1007/s00468-010-0530-x.

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Ruffner, Charles M., and Marc D. Abrams. "Relating land-use history and climate to the dendroecology of a 326-year-old Quercus prinus talus slope forest." Canadian Journal of Forest Research 28, no. 3 (March 1, 1998): 347–58. http://dx.doi.org/10.1139/x97-220.

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Dendroecology and land-use history were used to investigate the ecological history of a 326-year-old Quercus prinus L. forest. Quercus prinus, Castanea dentata (Marsh.) Borkh., and Pinus rigida Mill. dominated this talus slope prior to European settlement based on witness tree records. Oak species have exhibited continuous recruitment over three centuries probably in response to periodic fire and wind disturbances. While the stand escaped the direct impacts of timber cutting and the charcoal iron industry, the indirect effects of these land-use practices increased growth and recruitment. Different criteria were used for understory versus overstory trees to improve our detection of growth releases. Overall, major disturbances occurred approximately every 40 and 31 years before and after European settlement, respectively. This century, old-growth Q. prinus experienced marked growth increases coupled with high recruitment following the introduction of the chestnut blight (Cryphonectria parasitica (Murr.) Barr.) to the stand in 1909. Tree growth was also highly correlated with temperature and Palmer drought severity indices between 1895 and 1995. Climatic fluctuations in the 1820s-1830s and 1920s reduced radial growth and recruitment resulting in stem exclusion stages following regeneration pulses. Relating land-use history and climatic data to the dendroecology of this forest improved our understanding of its historical development.
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Dissertations / Theses on the topic "Dendroecology"

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Rauchfuss, Julia. "Software Review Autobox And Its Use In Dendroecology." Tree-Ring Society, 2011. http://hdl.handle.net/10150/622628.

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Vieira, Marcus Lanner. "Dendrocronologia de Hovenia dulcis, exótica e invasora nas florestas subtropicais brasileiras." Universidade do Vale do Rio dos Sinos, 2011. http://www.repositorio.jesuita.org.br/handle/UNISINOS/4767.

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FUNDEPE - Fundação Universitária para Desenvolvimento do Ensino e da Pesquisa
Petrobras - Petróleo Brasileiro S. A.
Hovenia dulcis Thunberg (Rhamnaceae) é uma espécie arbórea de origem asiática, comumente encontrada como invasora em formações florestais do sul do Brasil, onde compete com espécies arbóreas nativas em áreas de sucessão inicial e em clareiras no interior de florestas. Esta espécie, conhecida popularmente como uva-do-japão, perde completamente as folhas no período invernal, indicando um padrão fenológico estacional que estaria associado à formação de anéis de crescimento no lenho. Essas estruturas anatômicas marcam ciclos sazonais de atividade do câmbio vascular, fornecendo registros anuais da idade e do crescimento das plantas. Dessa forma, a existência de anéis de crescimento nesta espécie permitiria desenvolver estudos dendroecológicos, relevantes ao entendimento e manejo do seu processo de invasão. Neste estudo investigamos padrões de crescimento de H. dulcis através de séries temporais de largura de anéis de crescimento e suas relações com o clima regional. O estudo foi realizado em florestas ciliares de três arroios da bacia hidrográfica do rio dos Sinos, RS (29˚40”30’S; 50˚70”20’W), em cotas de 64 a 274m de altitude. Foram coletadas amostras de secções transversais do tronco de 49 indivíduos, com auxílio de um trado de incremento. As amostras foram preparadas datadas e medidas, gerando séries temporais de crescimento que foram submetidas a análises de correlação, regressão e ordenação para avaliar padrões de crescimento entre árvores e relações com séries históricas de temperatura atmosférica e precipitação. Os resultados demonstram que o crescimento de H. dulcis é sensível ao clima e apontam os principais fatores de influencias no crescimento. Destacamos a convergência no crescimento das árvores independente do seu local dentro da área de estudo. O sincronismo de crescimento expresso na cronologia apresentou sinais climáticos regionais atuando sobre a população. A série de crescimento regional média foi positivamente relacionada com a precipitação durante a primavera e o verão atual e temperatura de outono anterior. Isso significa que o crescimento de H. dulcis é sensível à baixa disponibilidade de água durante o período vegetativo e temperatura fria no outono restringe a duração de atividade de crescimento, reduzindo o crescimento na próxima temporada. Através do perfil de crescimento das árvores, reconhecemos árvores de crescimento rápido como sendo as que apresentam melhor o sinal comum de crescimento da população e mais sensíveis ao sinal regional. Identificamos também os indivíduos velhos, pequenos e de crescimento lento como representantes ruins do crescimento comum, pois estes são influenciados principalmente por fatores de micro sítio. Assim a datação precisa da idade dos indivíduos merece grande destaque, pois sugerem que medidas de diâmetro não são bons descritores de idade, não sendo esta medida adequada para estudos ecológicos que necessitem de estimativa de idade.
Hovenia dulcis Thunberg (Rhamnaceae) is a tree species from Asia invading forest formations in south Brazil, where it competes with native tree species in early succession areas and forest canopy gaps. The blueberry-japan shades its leaves in winter, indicating a seasonal phenological behavior that would be related to the formation of wood growth rings. This anatomical xylem structures mark seasonal cambium activity cycles, thus informing about tree age and annual growth. The formation of annual rings in H. dulcis would allow the development of dendroecological studies, relevant to understand and manage its invasion process. This study investigates long-term growth patterns of H. dulcis and relationships to regional climate through tree-ring analyses. The study was carried our in three riparian forests within the Dos Sinos river catchment (29˚40”30’S; 50˚70”20’W), between 64 and 274 m asl. Fourty nine trees were cored with an increment borer to obtain transversal trunk wood samples for tree ring analysis. The wood cores were surfaced, measured, cross-dated and detrended to obtain a annual growth index time series per tree. Regional temperature and precipitation series were obtained from modeled grid data-set. Growth patterns among trees and relationships with climate were explored through ordination, correlation and regression analyses. Trees from different riparian forests showed a similar growth pattern, indicative of a regional growth signal. The regional signal strength variation among trees did not varied in function of age but was directly related to tree size controlling age, indicating fast growing trees were more sensitive to such regional signal, probably because slow growing trees would be more influenced to site factors. The regional mean growth series was positively related to precipitation during current spring and summer and to temperature of previous autumn. It means H. dulcis growth is sensitive to low water availability during the vegetation period and cold temperature in autumn restricts the duration of growth activity, reducing growth in the next season.
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Guiterman, Christopher, and Christopher Guiterman. "Climate and Human Drivers of Forest Vulnerability in the US Southwest: Perspectives from Dendroecology." Diss., The University of Arizona, 2016. http://hdl.handle.net/10150/622981.

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The ongoing drought in the US Southwest (SW) has led to particularly large and severe wildfires, tree die-off events, insect outbreaks, and increased forest stress levels. These disturbances underscore the vulnerabilities of SW dry conifer forests to climate change and past land-uses. Climate projections show a clear upward trend in regional temperatures, which will lead to accelerated heat-related stressors and disturbances in the coming decades. Already, more than 20% of the dry conifer forests of the SW have been severely impacted. This number is likely to grow, but we lack a clear picture of where, when, and to what degree other forest areas will be affected. Here, I apply dendroecological methods to evaluate patterns and processes that might determine greater or lesser vulnerability in dry conifer forests. Much of this work stems from critical concerns voiced by the Navajo Forestry Department (NFD). Long-term and representative data are necessary for the NFD, as they are responsible for closely managing over 250,000 hectares of forests and woodlands for the traditional products and ecosystem services that their forests provide for the Navajo people. The first study takes a multi-century perspective on changing fire regimes across Navajo forests, and places current forest structure and recent severe events in a long-term context. We found that surface fires were frequent across the landscape from at least the late-1500s until 1880. Navajo settlement of the area began to affect the fire regimes with added small fires in some areas beginning in 1700. By 1832, the rise of traditional pastoralist practices and transhumant migrations reduced fire activity in areas of greater use. Conditions changed following the establishment of the Navajo reservation in 1868, as livestock herds grew rapidly and initiated a near-synchronous and widespread collapse of fire regimes across the study area by 1880. The legacies of this change in land use are greater forest densities and higher fuel loads in some areas, raising the vulnerability of the forest to more severe fires. The second study assesses one of the most dramatic long-term consequences of recent high-severity fires in the SW, the rapid post-fire transition of dry conifer forest to oak-dominated shrubfields. To assess probable successional trajectories and interactions with climate change of recently converted forests, we reconstructed the age structures and fire regimes of some of the largest and oldest shrubfields in the Jemez Mountains of northern New Mexico. We found that shrubfields are a resilient configuration to drought and fire, historically burning at the same rates and under similar climate as dry conifer forests. Dense shrubfields pose a significant challenge to conifer recruitment from competition effects, with our sites persisting for over 100 years in the absence of burning and through periods of favorable climate to conifers. Given future warming favoring oak over pine, and projected trends in fire activity and high-severity fire behavior, we expect much more forest area to convert to shrubfield, especially in the absence of restoration efforts to reduce crown fire potential.Finally, we evaluate landscape-scale variability in tree growth response to regional climate across the Navajo forest. Projections of climate-induced forest decline often omit upper-elevation and mesic sites because they are not represented in regional tree-ring chronology networks. We found that these stands had much lower response to 20th century droughts than mid to lower elevation stands, and that targeted tree-ring sites are consistently more correlated with regional climate. However, as temperature-driven atmospheric moisture demand has remained above average since ~1997 in the study area, the upper-elevation trees are now nearly as responsive to regional climate as lower elevation xeric sites, probably due to increased moisture limitations. Recent warming has thus synchronized tree growth to an unprecedented extent across this large landscape and regionally.
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Goins, Sean Michael. "Dynamics and Disturbance in an Old-Growth Forest Remnant in Western Ohio." University of Dayton / OhioLINK, 2012. http://rave.ohiolink.edu/etdc/view?acc_num=dayton1341941451.

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Backmeroff, Christa E. "Dendroecology, history and dynamics of mixed woodlands at the upper timberline of the central Italian Alps." Thesis, Bangor University, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.271282.

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Galván, Candela Juan Diego. "Long-term growth and functioning of high-elevation Pinus uncinata forests and trees inferred through dendroecology = Creixement i funcionament a llarg termini de boscos i individus de Pinus uncinata inferits mitjançant dendroecologia." Doctoral thesis, Universitat de Barcelona, 2014. http://hdl.handle.net/10803/132991.

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Iberian Pinus uncinata tree-growth variability and its responses to climate are analyzed by means of dendrochonological methods from an individual- to a population-level scale across its distribution area in the Iberian Peninsula. This multiple approach provides new knowledge about the site-tree-climate interactions at an individual scale, and about the species performance at a population scale. Age-related changes in sapwood area were the main drivers of BAI in mountain P. uncinata forests. Thus, any potential climate-induced effect on BAI will be mainly driven by sapwood production, which is mediated by tree age and altitude. Because slow-growing high-elevation trees get older than fast-growing low-elevation trees, we expect differential age-mediated BAI responses along the altitudinal gradient. Climate plays a secondary role in controlling TRWi variability among coexisting trees even in these high-elevation environments. Actually, altitude plays a major role affecting P. uncinata TRWi responses to climate at the site and tree scales. This suggests that the altitude-mediated decrease in air temperatures is the major driver of TRWi at both the site and tree levels determining the maximum elevation of the tree growth form. These results also stress that both (a) a tree-scale approach to quantify growth-index responses to climate and (b) a detailed characterization of the potential drivers of those individual tree responses are requisites for applying an individual-based framework in dendroecology. Following a population-based approach, a weakness of the theoretically temperature-sensitive TRW proxy to capture recent warming trends is observed. Instead, summer drought is increasingly influencing TRW along the 20th century, which agrees with observations from Iberian mountain forests. Rising temperatures might have led to an increase in drought stress of Pyrenean and Iberian high-elevation forests as has been observed in other Mediterranean similar ecosystems. We may be attending how a physiological threshold in terms of optimal temperature for growth is surpassed, reinforcing the role of drought as a plausible growth-limiting factor of Iberian high-elevation forests during the last decades. The intricate topography and diverse climate of the Mediterranean Basin produce varied and often opposite trend signs in dendrochronological proxies like TRW or BAI even between neighbouring sites, during the last decades. In spite of this local complexity, our findings reveal a pattern acting at synoptic scales where tree growth across the Mediterranean Basin is limited by drought or low water availability during the growing season.
La variabilitat del creixement de Pinus uncinata (pi negre) a la Península Ibèrica i les seues respostes al clima són analitzats a aquesta tesi mitjançant mètodes dendrocronològics, des d’una escala individual a una escala poblacional. Aquesta aproximació múltiple proveeix nous coneixements sobre les interaccions lloc-arbre-clima a escala individual, i sobre el comportament de la espècie a escala poblacional. Canvis a l’àrea d’albeca relacionats amb la edat van ser els principals factors de control de l’increment d’àrea basal (BAI) a aquests boscos de muntanya durant el segle XX. Per tant, els efectes potencials del clima sobre el BAI seran controlats principalment per la producció d’albeca, la qual al seu torn està influïda per la edat de l’arbre i la altitud. A més, arbres de creixement lent solen trobar-se en major proporció a altituds més elevades que arbres de creixement ràpid; com els primers solen ser més longeus, esperem unes respostes del BAI influïdes per la edat. El clima juga un paper secundari en el control de la variabilitat dels índexs d’amplària d’anell (TRWi) entre arbres coexistents, inclòs tractant-se d’aquests ecosistemes d’alta muntanya. Al contrari, l’altitud juga un paper prominent pel que fa a les respostes dels TRWi de P. uncinata al clima a escales de lloc i d’arbre. Açò suggereix que el decreixement en altitud de la temperatura de l’aire és el principal factor de control dels TRWi a ambdues escales. Aquests resultats també manifesten que (a) una aproximació dendrocronològica a nivell d’arbre per a quantificar les respostes dels TRWi al clima i (b) una caracterització detallada dels factors de control potencials d’aquestes respostes individuals són requisits per a fer servir una estratègia individual en dendroecologia. Seguint una aproximació poblacional, s’observa un debilitament de l’amplària d’anell (TRW) a l’hora de reflectir les tendències recents d’increment de temperatura. Per contra, la sequera estival està influint al TRW cada vegada més al llarg del segle XX, lo qual concorda amb observacions a altres boscos ibèrics de muntanya. L’increment recent de temperatura pot haver produït un augment de l’estrès per sequera als boscos pirenaics i ibèrics d’alta muntanya, com s’ha observat en altres ecosistemes mediterranis similars. D’aquesta manera, és possible que s’estiga depassant un llindar fisiològic des del punt de vista de la temperatura optima de creixement, reforçant el paper de la sequera com a plausible factor limitant del creixement a boscos ibèrics d’alta muntanya durant les darreres dècades. La topografia intricada i el clima divers de la Conca Mediterrània produeixen tendències variades recents als proxies dendrocronològics com ara TRW o BAI, sovint de signe oposat fins i tot entre llocs propers. Malgrat aquesta complexitat local, els nostres resultats posen de relleu un patró a escala sinòptica on el creixement arbori al llarg de la Conca Mediterrània està limitat per sequera o per baixa disponibilitat hídrica durant el període de creixement.
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Williams, Emma Clare, and Emma Clare Williams. "Prescribed Fire Can Increase Multi-Species, Regional-Scale Resilience to Increasing Climatic Water Deficit." Thesis, The University of Arizona, 2017. http://hdl.handle.net/10150/622901.

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Dry mixed conifer forests of southwestern North America are projected to be particularly vulnerable to ongoing persistent warm drought conditions, and related increases in wildfire frequency, size and severity, due in part to consequences of over a century of fire exclusion. Prescribed fire is applied actively in many landscapes to reduce hazardous fuel loads and continuity, restore forest community composition and structure, and increase tree resilience to drought stress. However, fire can also adversely affect tree growth by damaging cambial, root, and canopy tissues, leading to tradeoffs in the use of fire as a tool for forest resilience. Radial growth is an indicator of climatic and ecological stress and can thus provide a relative measure of resilience to stress and disturbances; but, the mechanisms driving tree resilience to prescribed fire and concurrent drought are poorly understood. Thinning effects of prescribed fire may increase tree resilience to drought by increasing water, light and nutrient availability and production of defense mechanisms. However, trends over the last century indicate warming temperatures are increasing tree sensitivity to fire by reducing post-fire growth (lower resilience) and increasing the likelihood of mortality. Trees can be resistant to fire exposure, and where growth changes occur they can be transient or persistent. We studied the interactions between tree- and stand-level fire effects on the growth responses of surviving Abies concolor, Pinus jefferyi, Pinus ponderosa, and Pseudotsuga menziesii over 24 years of variable climatic conditions in ten National Parks across the western and southwest United States. We used linear mixed effects models to identify mechanisms influencing resistance and resilience responses to fire and interannual climate, using climatic water deficit (CWD) as an index of climatic stress. Compared to pre-fire growth, trees exposed to fire increased growth during periods of greater water deficits. Tree growth responses were variable among and within species and size classes, but contingent on time-since-fire and the climate during the recovery period. Negative fire effects on tree resistance were generally transient, while climate and pre-existing stand conditions were persistent controls on tree resilience. These results suggest that antecedent and subsequent climate conditions modulate post-fire forest response. Consideration of climate variation could improve the strategic use of prescribed fire for tree resilience to drought, and a deeper understanding of factors contributing to prefire growth may elucidate the mechanisms driving post-fire growth responses.
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Bhuta, Arvind Aniel Rombawa. "A Denroecological Analysis of Disturbance of Remnant Pinus Palustris, Southeastern Virginia." Thesis, Virginia Tech, 2006. http://hdl.handle.net/10919/78137.

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Pinus palustris Miller (longleaf pine), in Virginia, is at the northernmost extent of its range. During presettlement times, this species occurred throughout the Piedmont and Coastal Plain of Virginia in pure and mixed stands, covering 607,000 hectares. This forest type has since been reduced to 81 hectares or 0.01% of its former range. Around 5,000 individual Pinus palustris remain on six sites in the coastal plains. Seacock Swamp and Everwoods are both sites known to have naturally regenerated Pinus palustris native to Virginia occurring in mixed-species stands. At both sites, I measured height and diameter of all Pinus palustris and cored individuals greater than 10 cm in diameter at breast height. A total of 71 trees were cored; the cores were crossdated and measured and crossdating was verified with the COFECHA program. A strong competition signal within the tree ring records at both sites signified the importance of stand dynamics on Pinus palustris in second-growth loblolly pine stands. These results are probably due to the mix of species within these stands and competition from loblolly pine as both the dominant understory and overstory species. Using Black and Abrams (2003) boundary line method, we calculated release and suppression events from the tree-ring record over the last century and found a very dynamic system. During the 1950s and 1960s, Seacock Swamp experienced major and moderate releases (23% moderate release and 18% major release in the 1950s and 33% moderate release and 49% major release in the 1960s) in response to a diameter-limit cut in 1953. Other major and moderate releases varied at both sites and may be attributed to different forest management practices that were in place throughout the last century however locating historical land use records to validate this was not possible at the present.
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Yao, Qichao, Peter M. Brown, Shirong Liu, Monique E. Rocca, Valerie Trouet, Ben Zheng, Haonan Chen, Yinchao Li, Duanyang Liu, and Xiaochun Wang. "Pacific-Atlantic Ocean influence on wildfires in northeast China (1774 to 2010)." AMER GEOPHYSICAL UNION, 2017. http://hdl.handle.net/10150/623055.

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Identification of effects that climate teleconnections, such as El Nino-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), and North Atlantic Oscillation (NAO), have on wildfires is difficult because of short and incomplete records in many areas of the world. We developed the first multicentury wildfire chronologies for northeast China from fire-scarred trees. Regional wildfires occurred every 7years from the 1700s to 1947, after which fire suppression policies were implemented. Regional wildfires occurred predominately during drought years and were associated with positive phases of ENSO and PDO and negative NAO. Twentieth century meteorological records show that this contingent combination of +ENSO/+PDO/-NAO is linked to low humidity, low precipitation, and high temperature during or before late spring fire seasons. Climate and wildfires in northeast China may be predictable based on teleconnection phases, although future wildfires may be more severe due to effects of climate change and the legacy of fire suppression.
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Leftwich, Samuel Joseph. "The resilience of forests to the urban ecosystem." Cleveland State University / OhioLINK, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=csu1631645306327862.

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Books on the topic "Dendroecology"

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Amoroso, Mariano M., Lori D. Daniels, Patrick J. Baker, and J. Julio Camarero, eds. Dendroecology. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-61669-8.

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Pompa-García, Marín, and J. Julio Camarero, eds. Latin American Dendroecology. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9.

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Eidgenössische Forschungsanstalt für Wald, Schnee und Landschaft., ed. Tree rings and environment dendroecology. Berne: Haupt, 1996.

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Wilford, D. J. Dendroecology: A guide for using trees to date geomorphic and hydrological events. [Victoria]: British Columbia, Ministry of Forests, Forest Science Program, 2005.

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Phipps, Richard, and Thomas Yanosky. Dendroecology: Principles and Practice. Ross Publishing, Incorporated, J., 2020.

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Baker, Patrick J., Mariano M. Amoroso, Lori D. Daniels, and J. Julio Camarero. Dendroecology: Tree-Ring Analyses Applied to Ecological Studies. Springer, 2018.

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Baker, Patrick J., Mariano M. Amoroso, Lori D. Daniels, and J. Julio Camarero. Dendroecology: Tree-Ring Analyses Applied to Ecological Studies. Springer, 2017.

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Dendroecology: A Guide for Using Trees to Date Geomorphic and Hydrological Events. Not Avail, 2005.

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Camarero, J. Julio, and Marín Pompa-García. Latin American Dendroecology: Combining Tree-Ring Sciences and Ecology in a Megadiverse Territory. Springer, 2020.

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Desta, Fekedulegn B., and United States. Forest Service. Northeastern Research Station., eds. Coping with multicollinearity: An example on application of principal components regression in dendroecology. Newtown Square, PA: U.S. Dept. of Agriculture, Forest Service, Northeastern Research Station, 2002.

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Book chapters on the topic "Dendroecology"

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Camarero, J. Julio. "Different Uncoupling of Growth and Water-Use Efficiency in Two Conifers Inhabiting Chilean Temperate Rainforests." In Latin American Dendroecology, 355–73. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_16.

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Rodríguez-Ramírez, Ernesto Chanes, and Isolda Luna-Vega. "Dendroecology as a Research Tool to Investigate Climate Change Resilience on Magnolia vovidesii, a Threatened Mexican Cloud Forest Tree Species of Eastern Mexico." In Latin American Dendroecology, 3–20. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_1.

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Guerrido, Claudia M., Ricardo Villalba, Mariano M. Amoroso, and Milagros Rodríguez-Catón. "Patterns of Tree Establishment Following Glacier-Induced Floods in Southern Patagonia." In Latin American Dendroecology, 225–46. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_10.

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Pompa-García, Marín, José Manuel Zúñiga-Vásquez, and Eduardo Treviño-Garza. "A Dendro-Spatial Analysis in Tree Growth Provides Insights into Forest Productivity." In Latin American Dendroecology, 247–62. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_11.

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Requena-Rojas, Edilson J., Doris B. Crispín-DelaCruz, Ginette Ticse-Otarola, Harold Rusbelth Quispe-Melgar, Janet G. Inga Guillen, Vladimir Camel Paucar, Anthony Guerra, Fressia Nathalie Ames-Martinez, and Mariano Morales. "Temporal Growth Variation in High-Elevation Forests: Case Study of Polylepis Forests in Central Andes." In Latin American Dendroecology, 263–79. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_12.

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Hadad, Martín Ariel, Julieta Gabriela Arco Molina, and Fidel Alejandro Roig. "Dendrochronological Study of the Xeric and Mesic Araucaria araucana Forests of Northern Patagonia: Implications for Ecology and Conservation." In Latin American Dendroecology, 283–315. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_13.

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Mundo, Ignacio A., Dino A. Palazzini, Antonio J. Barotto, Guillermo J. Martínez-Pastur, and Marcelo D. Barrera. "Dendroecology Applied to Silvicultural Management in the Southern Patagonian Forests: A Case Study from an Experimental Forest in Tierra del Fuego, Argentina." In Latin American Dendroecology, 317–30. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_14.

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Vettese, Evangelina Soledad, Ricardo Villalba, Ivonne Alejandra Orellana Ibáñez, and Pablo Luis Peri. "Tree-Growth Variations of Nothofagus antarctica Related to Climate and Land Use Changes in Southern Patagonia, Argentina." In Latin American Dendroecology, 331–54. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_15.

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Acosta-Hernández, Andrea Cecilia, Marín Pompa-García, Marcos González-Cásares, José Manuel Zúñiga-Vásquez, José Ciro Hernández-Díaz, José Rodolfo Goche-Telles, José Ángel Prieto-Ruíz, and Juan Abel Nájera-Luna. "How Drought Drives Seasonal Radial Growth in Pinus strobiformis from Northern Mexico." In Latin American Dendroecology, 21–36. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_2.

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Lisi, Claudio Sergio, Mariana Alves Pagotto, Claudio Roberto Anholetto, Francisco Carvalho Nogueira, Helberson Lima Santos, Clayane Matos Costa, Ítallo Romany Nunes Menezes, Fidel Alejandro Roig Juñet, and Mario Tommasiello Filho. "Dendroecological Studies with Cedrela odorata L., Northeastern Brazil." In Latin American Dendroecology, 37–59. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-36930-9_3.

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Conference papers on the topic "Dendroecology"

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Allen, Olivia, and Sean R. Cornell. "INVESTIGATION OF IMPACTS OF SEA-LEVEL RISE, STORM SURGE AND CLIMATE CHANGE ON MARITIME FORESTS ADJACENT TO CHINCOTEAGUE BAY, VIRGINIA USING DENDROECOLOGY TREE RING ANALYSIS." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-311363.

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Reports on the topic "Dendroecology"

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Fekedulegn, B. Desta, J. J. Colbert, R. R. ,. Jr Hicks, and Michael E. Schuckers. Coping with Multicollinearity: An Example on Application of Principal Components Regression in Dendroecology. Newtown Square, PA: U.S. Department of Agriculture, Forest Service, Northeastern Research Station, 2002. http://dx.doi.org/10.2737/ne-rp-721.

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