Gotowe bibliografie tematyczne / Rain forest

Gotowa bibliografia na temat „Rain forest”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 20 lutego 2023

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Artykuły w czasopismach na temat "Rain forest"

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Martin, K. C., i W. J. Freeland. "Herpetofauna of a northern Australian monsoon rain forest: seasonal changes and relationships to adjacent habitats". Journal of Tropical Ecology 4, nr 3 (sierpień 1988): 227–38. http://dx.doi.org/10.1017/s0266467400002790.

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ABSTRACTThe herpetofauna of a floodplain monsoon rain forest in northern Australia is composed primarily of species from non rain forest habitats. The majority of frog species use rain forest as a seasonal refuge, and there is a marked increase in numbers during the dry season. Faunal richness lies within limits expected on the basis of the length of the dry season and species richnesses of non-Australian faunas. There are few lizard species and an abundance of frog species (none of which is a rain forest specialist) in comparison to rain forest herpetofaunas in other tropical regions. The impoverished lizard fauna, and the paucity of rain forest specialists may be because (a) seasonal invasion of rain forest by frogs prevents evolution of, or colonization by, specialists or (b) rain forest specialists may not have been able to cross semiarid habitats separating the Northern Territory from eastern Australian rain forests. The herpetofaunas of monsoon forests in Cape York Peninsula may provide a means of distinguishing between these hypotheses.
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Xiang, Wen, Guang Fan Li i Yan Rong Li. "Hainan Tropical Rainforest Landslide Analysis and Prevention Measures". Applied Mechanics and Materials 638-640 (wrzesień 2014): 648–51. http://dx.doi.org/10.4028/www.scientific.net/amm.638-640.648.

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By Hainan tropical rainforest area geology, physiognomy, the characteristics of climate, tropical rain forest complex typhoon heavy rainfall weather conditions, and the characteristic of the tropical rainforest landslide occurred, researching and analyzing the relationship of among tropical rainforest landslide, tropical rain forest vegetation destruction the relationship ,the heavy rainfall and human engineering activities. Summed up the vegetation destruction, heavy rains and engineering activities of the three factors of coupling is the most important characteristics of tropical rain forests of landslide, and put forward reasonable tropical rainforest landslide protection and management measures.
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Behling, Hermann, i Raquel R. B. Negrelle. "Vegetation and pollen rain relationship from the tropical Atlantic rain forest in Southern Brazil". Brazilian Archives of Biology and Technology 49, nr 4 (lipiec 2006): 631–42. http://dx.doi.org/10.1590/s1516-89132006000500013.

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The relationship between the southern Brazilian tropical Atlantic lowland rain forest and modern pollen rain was studied by pollen traps. The study was carried out on a one hectare plot undisturbed rain forest of the reserve Volta Velha and two secondary forests, ± 50 and 7 years old. About 248 identified tree, shrub and herb species (excluding epiphytes) of 50 families were represented by 126 different pollen and spore types (including non-local taxa). The calculated average influx of pollen rain from the native Atlantic rain forest was 12465 pollen grains per cm² and year. The influx from the ± 50 years old and from the 7 years old secondary forest was relatively low (4112 and 3667 grains per cm² and year, respectively) compared to the undisturbed rain forest. The occurrence of pollen grains of herbs and fern spores were significantly higher in the secondary forests than in the undisturbed rain forest.
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Whitehouse, John F. "East Australian Rain-forests: A Case-study in Resource Harvesting and Conservation". Environmental Conservation 18, nr 1 (1991): 33–43. http://dx.doi.org/10.1017/s0376892900021263.

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Human interactions with rain-forest on the Australian continent have played, and will continue to play, a vital role in their distribution and survival. The presence and significance of rain-forest in Australia lies in the evolutionary history of the Australian plate since the break-up of the Gondwanan supercontinent. Its continued survival and distribution illustrates and encapsulates the history of plant evolution and biogeography in Australia.Since human arrival in Australia at least 40,000 years ago, human interactions with rain-forest have been marked by a number of phases — ranging from Aboriginal use of rain-forest resources to the impetus given by the hunt for the prized Red Cedar, and from the early European settlement on the east coast of Australia in the midto late-19th century to the wholesale clearing of rain forests for agricultural settlement and dairying in the late 19th century. In more modern times, human interactions with rain-forest have focused on adapting forest management techniques to rain-forest logging, restructuring the native forest timber industry in the face of mechanization, changing markets and resource constraints, convulsions as a result of conservationist challenges in Terania Creek and Daintree, and finally the implications of conserving rain-forests in the context of natural processes including fire, climate change, and the impact of human visitors and their recreation.The course of the controversies over rain-forest conservation in Australia has meant that rain-forest logging either has been dramatically curtailed or is in the process of generally ceasing. The protection of rainforests from logging and forestry operations in the future seems secure, given the widespread community support for rain-forest conservation. Threats to rain-forest conservation in the future are likely to be found in more subtle processes: the impact of fire regimes on the spread and contractions of rain-forests, the impacts of exotic species such as Lantana (Lantana camara) and Camphor Laurel (Cinnamomum camphora), the impacts of human uses through tourism and recreation, the diminution of the viability of isolated pockets by ‘edge effects’, and the damage to the remaining stands on freehold property by conflicting land-uses.Overlying all of these potential threats is the impact of global climate change. Climate change since the Tertiary has reduced the once widespread rain-forest communities of Australia practically to the status of relicts in refugia. Will the remaining rain-forests be able to withstand the projected human-induced climate changes of the future?
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Travis, John. "Rain Forest Primeval?" Science News 161, nr 26 (29.06.2002): 403. http://dx.doi.org/10.2307/4013494.

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Proctor, John. "Tropical rain forest". Progress in Physical Geography: Earth and Environment 11, nr 3 (wrzesień 1987): 406–18. http://dx.doi.org/10.1177/030913338701100307.

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Proctor, John. "Tropical rain forest". Progress in Physical Geography: Earth and Environment 12, nr 3 (wrzesień 1988): 405–20. http://dx.doi.org/10.1177/030913338801200305.

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Schneider, David. "Rain Forest Crunch". Scientific American 274, nr 3 (marzec 1996): 19. http://dx.doi.org/10.1038/scientificamerican0396-19.

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Banfai, Daniel S., i David M. J. S. Bowman. "Drivers of rain-forest boundary dynamics in Kakadu National Park, northern Australia: a field assessment". Journal of Tropical Ecology 23, nr 1 (styczeń 2007): 73–86. http://dx.doi.org/10.1017/s0266467406003701.

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Understanding the causes of savanna–forest dynamics is vital as small but widespread changes in the extent of tropical forests can have major impacts on global climate, biodiversity and human well-being. Comparison of aerial photographs for 50 rain-forest patches in Kakadu National Park had previously revealed a landscape-wide monotonic expansion of rain-forest boundaries between 1964 and 2004. Here floristic, structural, environmental and disturbance attributes of the changes were investigated by sampling 588 plots across 30 rain-forest patches. Areas that had changed from savanna to rain forest were associated with a significantly higher abundance of rain-forest trees and less grasses, relative to stable savanna areas. Ordination analyses showed that overall floristic composition was not significantly different between newly established rain forest and longer established rain forest. Generalized linear models also indicated that contemporary levels of disturbance (fire and feral animal impact) and environmental variables (slope and soil texture) were poor predictors of historical vegetation change. We concluded that (1) the rain-forest boundaries are highly dynamic at the decadal scale; (2) rain-forest expansion is consistent with having been driven by global environmental change phenomena such as increases in rainfall and atmospheric CO2; and (3) expansion will continue if current climatic trends and management conditions persist.
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Kuusipalo, Jussi, Jyrki Kangas i Lauri Vesa. "Sustainable Forest Management in Tropical Rain Forests". Journal of Sustainable Forestry 5, nr 3-4 (10.04.1997): 93–118. http://dx.doi.org/10.1300/j091v05n03_06.

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Rozprawy doktorskie na temat "Rain forest"

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Manokaran, N. "Population dynamics of tropical forest trees". Thesis, Available from the University of Aberdeen Library and Historic Collections Digital Resources, 1988. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=59678.

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Nascimento, Marcelo T. "A monodominant rain forest on Maraca Island, Roraima, Brazil : forest structure and dynamics". Thesis, University of Stirling, 1994. http://hdl.handle.net/1893/21893.

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A forest type dominated by Peltogyne gracilipes Ducke (Caesalpiniaceae) occurs on Maraca Island on a range of soil types. Maraca is located in Roraima State (Brazil) in the Rio Uraricoera and has an area of about 100,000 ha. This study compares the structure and floristic composition of the Peltogyne forest with the most widespread lowland forest type on Maraca and investigates some factors that could be involved in the persistent monodominance of Peltogyne. Three 0.25 ha plots were set up in each of three forest types: Peltogyne-rich forest (PRF), Peltogyne-poor forest (PPF) and forest without Peltogyne (FWP). Within each plot all trees (~ 10 cm dbh) were recorded. Seedlings and saplings were sampled in sub-plots of 2 m x 1 m (seedlings) and 4 m x 4 m (saplings). In the PPF and FWP, Sapotaceae were the most important family with the highest dominance and relative density values. Caesalpiniaceae showed high values in the PRF and PPF. Licania kunthiana, Pradosia surinamensis and Simarouba amara occurred in the forest types. Peltogyne dominated had 20% of stems and 53% of the trees ~ 10 cm dbh, and 91% of the canopy layer the canopy in total basal stems and 97% in all the the PRF and area of all of the total basal area of individuals > 50 cm dbh. In PPF, Lecythis corrugata and Tetragastris panamensis were the most abundant species, followed by Peltogyne. In the FWP the most abundant trees (~ 10 cm dbh) were L. kunthiana and P. surinamensis. In general, Peltogyne had low rates of seed predation and herbivory, but suffered locally high levels of damage to its seeds by leaf-cutter ants and was once observed to have an infestation of larvae of the moth Eulepidotis phrygionia on its young leaves. Peltogyne had no allelopathic effects on tested species and had VA mycorrhizal associations. Its occurrence remains unexplained but is most clearly correlated with soil magnesium.
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Ramdass, Indarjit. "Modelling forest dynamics and management of natural tropical rain forests". Thesis, University of Edinburgh, 1987. http://hdl.handle.net/1842/11890.

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Poels, R. L. H. "Soils, water and nutrients in a forest ecosystem in Suriname". Wageningen : Agricultural University, 1987. http://catalog.hathitrust.org/api/volumes/oclc/23819734.html.

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Valencia, Niels. "Ecology of forests on the western slopes of the Peruvian Andes". Thesis, University of Aberdeen, 1990. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=128343.

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Dry cloud forests on the western slopes of the Peruvian Andes were mapped from aerial photographs, 306 stands being recorded from 4o50'S to 12o47'S. The frequency and area of these stands, as well as most parameters analyzed in the eight sample sites, show a steep decreasing latitudinal trend and are strongly correlated with the latitudinal rainfall gradient. The mean area of the forest stands decreases from 115 ha in northern Peru to 42 ha in central Peru. The number of species recorded decreases along the study area from 52 to 13 and there is a well defined latitudinal sequence of species. Mean density and basal area per hectare of stems ≥10 cm gbh decreases from 2995 individuals and 79.91 m^2 in the north to 500 individuals and 17.27 m^2 in central Peru. The vertical structure is similar throughout the study area, emergent trees reaching on average 22 m and the main canopy 12 m in the north and 13 m and 7 m respectively in central Peru. Regeneration is very active in northern Peru. Juveniles have been found for a high proportion of species, including all common ones, and most species show a logarithmic decline in number of stems with increasing girth. There is a steep decreasing trend towards central Peru, where few species regenerate, mostly shrubs. The pattern found may be the result of the combined effect of grazing and a climatic change towards drier conditions evidenced in the regeneration pattern of most sites.
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Hogan, Anthony David. "Australia's native forest and rainforest timber usage and the plantation strategy alternative /". Title page, table of contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09ENV/09envh714.pdf.

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Tomlinson, Francis J. "Do harvesting impacts determine patterns of non-forest vegetation in Dipterocarp Forest in Sabah 15 years post logging?" Available from the University of Aberdeen Library and Historic Collections Digital Resources, 2009. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=59623.

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Abebe, Tarekegn. "The influence of selective logging on residual stand and regeneration in a rain forest in southwestern Ethiopia /". Umeå : Swedish University of Agricultural Sciences, 2003. http://diss-epsilon.slu.se/archive/00000213/.

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Thesis (doctoral)--Swedish University of Agricultural Sciences, 2003.
Thesis documentation sheet inserted. Appendix includes five manuscripts submitted for publication elsewhere, four co-authored with others. Includes bibliographical references.
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Hausmann, Franziska. "The utility of linear riparian rainforest for vertebrates on the Atherton and Evelyn Tablelands, North Queensland /". Click here to access, 2004. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20050115.105740.

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Thesis (M.Phil.) -- Griffith University, 2004.
Facsimile of the author's original dissertation. Pagination of document: x, 121 leaves. Includes bibliographical references. Also available online via the World Wide Web.
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Grainger, A. "The future role of the tropical rain forests in the world forest economy". Thesis, University of Oxford, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.377888.

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Książki na temat "Rain forest"

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Michael, George. Rain forest. Mankato, Minn: Creative Education, 1992.

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Macdonald, Fiona. Rain forest. Austin, Tex: Raintree Steck-Vaughn, 1994.

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Macdonald, Fiona. Rain forest. New York: F. Watts, 2000.

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Greenwood, Elinor. Rain forest. New York: Dorling Kindersley Pub., 2001.

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George, Michael. Rain forest. Mankato, Minn: Creative Education, 1992.

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1946-, Morris Neil, i Hulse Gillian ill, red. Rain forest. New York: F. Watts, 1994.

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Rain forest. New York: FUNFAX, 1998.

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Morris, Ting. Rain forest. North Mankato, Minn: Sea-to-Sea Publications, 2007.

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Barbara, Taylor. Rain forest. New York: Funfax, 1998.

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Rain forest. New York: Farrar, Strauss, and Giroux, 1988.

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Części książek na temat "Rain forest"

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Znoj, Heinzpeter, Rahel Jud i Yudi Bachrioktora. "Rain forest anomy". W The Commons in a Glocal World, 414–34. Abingdon, Oxon ; New York, NY : Routledge, 2019.: Routledge, 2019. http://dx.doi.org/10.4324/9781351050982-25.

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Jacobs, Marius. "Forest and Man". W The Tropical Rain Forest, 250–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72793-1_19.

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Mabberley, D. J. "The Tropical Rain Forest". W Tropical Rain Forest Ecology, 1–16. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-3672-7_1.

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Mabberley, D. J. "Traditional Rain-Forest Use". W Tropical Rain Forest Ecology, 205–20. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-3672-7_8.

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Mabberley, D. J. "The Tropical Rain Forest". W Tropical Rain Forest Ecology, 1–16. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3048-6_1.

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Mabberley, D. J. "Traditional Rain-Forest Use". W Tropical Rain Forest Ecology, 205–20. Dordrecht: Springer Netherlands, 1992. http://dx.doi.org/10.1007/978-94-011-3048-6_8.

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Cook, Suzanne. "The Lacandon Rain Forest". W The Forest of the Lacandon Maya, 13–24. Boston, MA: Springer US, 2016. http://dx.doi.org/10.1007/978-1-4614-9111-8_3.

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Collins, N. Mark, Jeffrey A. Sayer i Timothy C. Whitmore. "Natural Rain Forest Management". W The Conservation Atlas of Tropical Forests Asia and the Pacific, 43–50. London: Palgrave Macmillan UK, 1991. http://dx.doi.org/10.1007/978-1-349-12030-7_6.

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Mabberley, D. J. "The Changing Forest Today". W Tropical Rain Forest Ecology, 221–63. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-3672-7_9.

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Jacobs, Marius. "Primary and Secondary Forest". W The Tropical Rain Forest, 89–99. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-72793-1_8.

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Streszczenia konferencji na temat "Rain forest"

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Florian, K., P. Kostas, H. Irena i H. Dirk. "Forest Height Estimation in Tropical Rain Forest using Pol-InSAR Techniques". W 2006 IEEE International Symposium on Geoscience and Remote Sensing. IEEE, 2006. http://dx.doi.org/10.1109/igarss.2006.567.

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Oliver, Christopher J., Kevin O. Grover, Sidnei Sant'Anna i Corina da Costa Freitas. "Use of satellite SAR for monitoring rain forest". W Remote Sensing, redaktor Francesco Posa. SPIE, 1999. http://dx.doi.org/10.1117/12.373160.

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Carlos Marchi, Luiz, Serge Le Failler i Jean Jacques Postel. "3-D Seismic Acquisition In The Amazonia Rain Forest". W 6th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 1999. http://dx.doi.org/10.3997/2214-4609-pdb.215.sbgf155.

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Goffart, A., S. Matesco, A. Rocher, M. Jacquet i J. F. Vidalie. "Environmental Management Of Drilling Operations In Bolivian Rain Forest". W SPE Health, Safety and Environment in Oil and Gas Exploration and Production Conference. Society of Petroleum Engineers, 1996. http://dx.doi.org/10.2118/37034-ms.

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Westgate, James W. "A MECO RAIN FOREST/MANGROVE COMMUNITY FROM LAREDO, TEXAS". W 51st Annual GSA South-Central Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017sc-289584.

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TAMAI, KOJI. "FOREST MANAGEMENT TO MITIGATE DISASTERS CAUSED BY HEAVY RAIN". W WATER AND SOCIETY 2021. Southampton UK: WIT Press, 2021. http://dx.doi.org/10.2495/ws210061.

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Maderkova, Lucia. "RAIN FACTOR CALCULATION - COMPARISON OF DIFFERENT METHODOLOGIES WHICH CONSIDER DATA AVAIBILITY". W 13th SGEM GeoConference on WATER RESOURCES. FOREST, MARINE AND OCEAN ECOSYSTEMS. Stef92 Technology, 2013. http://dx.doi.org/10.5593/sgem2013/bc3/s13.022.

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K Abdul Hamid, Abdul Aziz, R. U. Gobithaasan, Sumazly Sulaiman i Nur Syazwani. "Tropical Rain Forest Monitoring and Evaluation using Image Segmentation Approach". W The 2nd World Congress on Electrical Engineering and Computer Systems and Science. Avestia Publishing, 2016. http://dx.doi.org/10.11159/mvml16.106.

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Anselmo-Moreira, F., J. Gagliano i CM Furlan. "Anticholinesterase activity of an endemic Atlantic rain forest bamboo species". W 67th International Congress and Annual Meeting of the Society for Medicinal Plant and Natural Product Research (GA) in cooperation with the French Society of Pharmacognosy AFERP. © Georg Thieme Verlag KG, 2019. http://dx.doi.org/10.1055/s-0039-3399956.

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Vaca, Cesar Cisneros, i Christiaan van der Tol. "Sensitivity of Sentinel-1 to Rain Stored in Temperate Forest". W IGARSS 2018 - 2018 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2018. http://dx.doi.org/10.1109/igarss.2018.8517859.

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Raporty organizacyjne na temat "Rain forest"

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Nicholls, David, i Trista Patterson. Greenhouse gas emissions versus forest sequestration in temperate rain forests—a southeast Alaska analysis. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 2015. http://dx.doi.org/10.2737/pnw-gtr-918.

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Carrasco, C. E., H. J. Alvarez, N. Ortiz, M. Bisbal, W. Arias, C. Baerga i T. C. Hazen. Multiple antibiotic resistant Escherichia coli from a tropical rain forest stream. Office of Scientific and Technical Information (OSTI), grudzień 1988. http://dx.doi.org/10.2172/666133.

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Perez-Rosas, N., i T. C. Hazen. Survival and distribution of Vibrio cholerae in a tropical rain forest stream. Office of Scientific and Technical Information (OSTI), grudzień 1988. http://dx.doi.org/10.2172/666266.

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Oberbauer, S. F. Current and Future Carbon Budgets of Tropical Rain Forest: A Cross Scale Analysis. Final Report. Office of Scientific and Technical Information (OSTI), styczeń 2004. http://dx.doi.org/10.2172/825088.

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Nowacki, Gregory J., i Marc G. Kramer. The effects of wind disturbance on temperate rain forest structure and dynamics of southeast Alaska. Portland, OR: U.S. Department of Agriculture, Forest Service, Pacific Northwest Research Station, 1998. http://dx.doi.org/10.2737/pnw-gtr-421.

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van der Sanden, J. J. RADARSAT-1 Applied to the Mapping of Tropical Rain Forest: A Case Study in Guyana. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2002. http://dx.doi.org/10.4095/219865.

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Douglas, Thomas, Merritt Turetsky i Charles Koven. Increased rainfall stimulates permafrost thaw across a variety of Interior Alaskan boreal ecosystems. Engineer Research and Development Center (U.S.), czerwiec 2021. http://dx.doi.org/10.21079/11681/41050.

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Earth’s high latitudes are projected to experience warmer and wetter summers in the future but ramifications for soil thermal processes and permafrost thaw are poorly understood. Here we present 2750 end of summer thaw depths representing a range of vegetation characteristics in Interior Alaska measured over a 5-year period. This included the top and third wettest summers in the 91-year record and three summers with precipitation close to mean historical values. Increased rainfall led to deeper thaw across all sites with an increase of 0.7 ± 0.1 cm of thaw per cm of additional rain. Disturbed and wetland sites were the most vulnerable to rain-induced thaw with ~1 cm of surface thaw per additional 1 cm of rain. Permafrost in tussock tundra, mixed forest, and conifer forest was less sensitive to rain-induced thaw. A simple energy budget model yields seasonal thaw values smaller than the linear regression of our measurements but provides a first-order estimate of the role of rain-driven sensible heat fluxes in high-latitude terrestrial permafrost. This study demonstrates substantial permafrost thaw from the projected increasing summer precipitation across most of the Arctic region.
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Lane, Erin, i Kate MacFarland. 360o of Silvopasturing to Adapt to Climate Change. USDA Northeast Climate Hub, sierpień 2018. http://dx.doi.org/10.32747/2018.6937342.ch.

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Climate change is already impacting farm and forest lands throughout the northeastern United States. Temperatures are increasing and more rain is falling all at once with dry periods in between. With these changes comes greater variation and uncertainty in crop and livestock production. Without modifying management, agricultural profits may decline
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Brandt, Leslie A., Cait Rottler, Wendy S. Gordon, Stacey L. Clark, Lisa O'Donnell, April Rose, Annamarie Rutledge i Emily King. Vulnerability of Austin’s urban forest and natural areas: A report from the Urban Forestry Climate Change Response Framework. U.S. Department of Agriculture, Northern Forests Climate Hub, październik 2020. http://dx.doi.org/10.32747/2020.7204069.ch.

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The trees, developed green spaces, and natural areas within the City of Austin’s 400,882 acres will face direct and indirect impacts from a changing climate over the 21st century. This assessment evaluates the vulnerability of urban trees and natural and developed landscapes within the City Austin to a range of future climates. We synthesized and summarized information on the contemporary landscape, provided information on past climate trends, and illustrated a range of projected future climates. We used this information to inform models of habitat suitability for trees native to the area. Projected shifts in plant hardiness and heat zones were used to understand how less common native species, nonnative species, and cultivars may tolerate future conditions. We also assessed the adaptability of planted and naturally occurring trees to stressors that may not be accounted for in habitat suitability models such as drought, flooding, wind damage, and air pollution. The summary of the contemporary landscape identifies major stressors currently threatening trees and forests in Austin. Major current threats to the region’s urban forest include invasive species, pests and disease, and development. Austin has been warming at a rate of about 0.4°F per decade since measurements began in 1938 and temperature is expected to increase by 5 to 10°F by the end of this century compared to the most recent 30-year average. Both increases in heavy rain events and severe droughts are projected for the future, and the overall balance of precipitation and temperature may shift Austin’s climate to be more similar to the arid Southwest. Species distribution modeling of native trees suggests that suitable habitat may decrease for 14 primarily northern species, and increase for four more southern species. An analysis of tree species vulnerability that combines model projections, shifts in hardiness and heat zones, and adaptive capacity showed that only 3% of the trees estimated to be present in Austin based on the most recent Urban FIA estimate were considered to have low vulnerability in developed areas. Using a panel of local experts, we also assessed the vulnerability of developed and natural areas. All areas were rated as having moderate to moderate-high vulnerability, but the underlying factors driving that vulnerability differed by natural community and between East and West Austin. These projected changes in climate and their associated impacts and vulnerabilities will have important implications for urban forest management, including the planting and maintenance of street and park trees, management of natural areas, and long-term planning.
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Jimenez, Jose-Luis, Douglas A. Day, Scot T. Martin, Saewung Kim, James Smith, Rodrigo Souza i Henry Barbosa. Brazil-USA Collaborative Research: Modifications by Anthropogenic Pollution of the Natural Atmospheric Chemistry and Particle Microphysics of the Tropical Rain Forest During the GoAmazon Intensive Operating Periods (IOPs). Office of Scientific and Technical Information (OSTI), sierpień 2017. http://dx.doi.org/10.2172/1374492.

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