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  • 1
    Online Resource
    Online Resource
    Newark :American Geophysical Union,
    Keywords: Climatic changes -- Amazon River Region. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (576 pages)
    Edition: 1st ed.
    ISBN: 9781118672365
    Series Statement: Geophysical Monograph Series ; v.186
    DDC: 577.34/1409811
    Language: English
    Note: Intro -- Title Page -- Contents -- Preface -- Section I: People and Land Change -- People and Environment in Amazonia: The LBA Experience and Other Perspectives -- The Changing Rates and Patterns of Deforestation and Land Use in Brazilian Amazonia -- Selective Logging and Its Relation to Deforestation -- The Spatial Distribution and Interannual Variability of Fire in Amazonia -- The Expansion of Intensive Agriculture and Ranching in Brazilian Amazonia -- Scenarios of Future Amazonian Landscapes: Econometric and Dynamic Simulation Models -- Road Impacts in Brazilian Amazonia -- Small Farmers and Deforestation in Amazonia -- Section II: Atmosphere and Climate -- Understanding the Climate of Amazonia: Progress From LBA -- Characteristics of Amazonian Climate: Main Features -- The Amazonian Boundary Layer and Mesoscale Circulations -- Natural Volatile Organic Compound Emissions From Plants and Their Roles in Oxidant Balance and Particle Formation -- Biomass Burning in Amazonia: Emissions, Long-Range Transport of Smoke and Its Regional and Remote Impacts -- Aerosol Particles in Amazonia: Their Composition, Role in the Radiation Balance, Cloud Formation, and Nutrient Cycles -- Modeling the Regional and Remote Climatic Impact of Deforestation -- Evapotranspiration -- Global Warming and Climate Change in Amazonia: Climate-Vegetation Feedback and Impacts on Water Resources -- Section III: Terrestrial Ecosystems -- Biogeochemistry and Ecology of Terrestrial Ecosystems of Amazonia -- Nutrient Limitations to Secondary Forest Regrowth -- The Maintenance of Soil Fertility in Amazonian Managed Systems -- Sources and Sinks of Trace Gases in Amazonia and the Cerrado -- The Production, Storage, and Flow of Carbon in Amazonian Forests -- Changes in Amazonian Forest Biomass, Dynamics, and Composition, 1980-2002. , Ecosystem Carbon Fluxes and Amazonian Forest Metabolism -- The Regional Carbon Budget -- The Effects of Drought on Amazonian Rain Forests -- Soil Carbon Dynamics -- Ecophysiology of Forest and Savanna Vegetation -- Section IV: Surface Water -- Surface Waters in Amazonia: Key Findings and Perspectives -- The Role of Rivers in the Regional Carbon Balance -- Water and Chemical Budgets at the Catchment Scale Including Nutrient Exports From Intact Forests and Disturbed Landscapes -- Floodplain Ecosystem Processes -- Effects of Climatic Variability and Deforestation on Surface Water Regimes -- Section V: Conclusions and Vision for the Future -- Results From LBA and a Vision for Future Amazonian Research -- Index.
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  • 2
    Publication Date: 2024-04-17
    Description: Phenology is the study of reoccurring events during a year or season. It can be linked to the behavior of animals, such as phases of mating, breeding, or movement and to events such as green-up, bud burst, flowering, or senescence when referring to vegetation, as a response to changing environmental factors throughout a season. While these changes can be tracked on the level of individual species, their observation is usually restricted to small spatial extents. To broaden the extent of the observed area remote sensing data have been proven useful. As remote sensing data capture the seasonal change rather on a pixel than on a species level, they enable to analyze the phenology of the observed vegetation on a different scale, which is known as land surface phenology. Land surface phenological metrics that can, for example, be derived from time series of vegetation indices, allow to analyze the observed spatial and temporal patterns in relation to ecosystem processes (e.g., primary productivity). Subsequently, the derived metrics can be grouped based on their similarities into land surface phenological archetypes (LSP), defined as areas with comparable phenologies. However, the spatial resolution of the data used is crucial, which becomes even more critical when looking at heterogeneous ecosystems such as the Brazilian savanna, known as the Cerrado. The Cerrado covers an extent of approximately 2 mio. km², hosts many endemic species and is considered as a biodiversity hotspot that provides several ecosystem services of national and even global importance. However, due to a lack of extensive conservation regulations the Cerrado is prone to land cover changes for agricultural expansion, highlighting the need for detailed mapping and monitoring approaches. To reveal and analyze the spatial patterns of the remaining share of natural vegetation based on their land surface phenology, we analyzed a dense 8-day time series of combined enhanced vegetation data derived from Landsat 7 ETM+ and Landsat 8 images. Data gaps that were due to cloud contamination or sensor errors were filled using a radial basis convolution filter, enabling to subsequently derive phenological metrics for the season 2013/2014 using TIMESAT (Eklundh and Jönsson 2017). As these variables, such as start and end of season, amplitude or the base value, relate to the seasonality and primary productivity of the observed vegetation, we clustered them based on their similarities and defined 8 land surface phenological archetypes (LSP) of the Cerrado. The GeoTiff file contains the 8 LSPs that are explained in detail in Schwieder et al. in prep. For further questions please contact Marcel Schwieder. Class labels: 0 = Unclassified 1 = FORMBMS 2 = SAFORMS 3 = FORHBLS 4 = GLSAVLB 5 = GLSAVHB 6 = FORHBHS 7 = VEGINMS 8 = VEGINLS
    Keywords: Cerrado; Cerrado_ecosystem_funct_types; Conservation; Land surface phenology; remote sensing; SAT; Satellite remote sensing; Timesat
    Type: Dataset
    Format: image/tiff, 365.1 MBytes
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  • 3
    ISSN: 1365-2486
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Energy, Environment Protection, Nuclear Power Engineering , Geography
    Notes: The majority of deforested land in the Amazon Basin has become cattle pasture, making forest-to-pasture conversion an important contributor to the carbon (C) and climate dynamics of the region. However, our understanding of biogeochemical dynamics in pasturelands remains poor, especially when attempting to scale up predictions of C cycle changes. A wide range of pasture ages, soil types, management strategies, and climates make remote sensing the only realistic means to regionalize our understanding of pasture biogeochemistry and C cycling over such an enormous geographic area. However, the use of remote sensing has been impeded by a lack of effective links between variables that can be observed from satellites (e.g. live and senescent biomass) and variables that cannot be observed, but which may drive key changes in C storage and trace gas fluxes (e.g. soil nutrient status). We studied patterns in canopy biophysical–biochemical properties and soil biogeochemical processes along pasture age gradients on two important soil types in the central Amazon. Our goals were to (1) improve our understanding of the plot-scale biogeochemical dynamics of this land-use change, (2) evaluate the effects of pasture development on two contrasting soil types (clayey Oxisols and sandy Entisols), and (3) attempt to use remotely sensed variables to scale up the site-specific variability in biogeochemical conditions of pasturelands.The biogeochemical analyses showed that (1) aboveground and soil C stocks decreased with pasture age on both clayey and sandy soils, (2) declines in plant biomass were well correlated with declines in soil C and with available phosphorus (P) and calcium (Ca), and (3) despite low initial values for total and available soil P, ecosystem P stocks declined further with pasture age, as did a number of other nutrients. Spectral mixture analysis of Landsat imagery provided estimates of photosynthetic vegetation (PV) and non-photosynthetic vegetation (NPV) that were highly correlated with field measurements of these variables and plant biomass. In turn, the remotely sensed sum PV+NPV was well correlated with the changes in soil organic carbon and nitrogen, and available P and Ca. These results suggest that remote sensing can be an excellent indicator of not only pasture area, but of pasture condition and C storage, thereby greatly improving regional estimates of the environmental consequences of such land-use change.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of springer for personal use, not for redistribution. The definitive version was published in Biogeochemistry 105 (2011): 19-35, doi:10.1007/s10533-011-9574-2.
    Description: Stream discharge-concentration relationships are indicators of terrestrial ecosystem function. Throughout the Amazon and Cerrado regions of Brazil rapid changes in land use and land cover may be altering these hydrochemical relationships. The current analysis focuses on factors controlling the discharge-calcium (Ca) concentration relationship since previous research in these regions has demonstrated both positive and negative slopes in linear log10discharge-log10Ca concentration regressions. The objective of the current study was to evaluate factors controlling stream discharge-Ca concentration relationships including year, season, stream order, vegetation cover, land use, and soil classification. It was hypothesized that land use and soil class are the most critical attributes controlling discharge-Ca concentration relationships. A multilevel, linear regression approach was utilized with data from 28 streams throughout Brazil. These streams come from three distinct regions and varied broadly in watershed size (〈1 to 〉106 ha) and discharge (10-5.7 to 103.2 m3 sec-1). Linear regressions of log10Ca versus log10discharge in 13 streams have a preponderance of negative slopes with only two streams having significant positive slopes. An ANOVA decomposition suggests the effect of discharge on Ca concentration is large but variable. Vegetation cover, which incorporates aspects of land use, explains the largest proportion of the variance in the effect of discharge on Ca followed by season and year. In contrast, stream order, land use, and soil class explain most of the variation in stream Ca concentration. In the current data set, soil class, which is related to lithology, has an important effect on Ca concentration but land use, likely through its effect on runoff concentration and hydrology, has a greater effect on discharge-concentration relationships.
    Description: This research was supported by grant #’s NCC5-686 and NNG06GE88A of NASA’s Terrestrial Ecology Program as part of the Large-scale Biosphere-Atmosphere Experiment in Amazonia (LBA-ECO) project.
    Repository Name: Woods Hole Open Access Server
    Type: Preprint
    Format: application/pdf
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  • 5
    Publication Date: 2019-04-01
    Keywords: ddc:300
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: English
    Type: bookpart , doc-type:bookPart
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  • 6
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