125 research outputs found

    Application of Geographically Weighted Regression to Investigate the Impact of Scale on Prediction Uncertainty by Modelling Relationship between Vegetation and Climate

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    Scale-dependence of spatial relationship between vegetation and rainfall in Central Sulavesi has been modelled using Normalized Difference Vegetation Index (NDVI) and rainfall data from weather stations. The modelling based on application of two statistical approaches: conventional ordinary least squares (OLS) regression, and geographically weighted regression (GWR). The analysis scales ranged from the entire study region to spatial unities with a size of 750*750 m. The analysis revealed the presence of spatial non-stationarity for the NDVI-precipitation relationship. The results support the assumption that dealing with spatial non-stationarity and scaling down from regional to local modelling significantly improves the model’s accuracy and prediction power. The local approach also provides a better solution to the problem of spatially autocorrelated errors in spatial modelling

    Modified Light Use Efficiency Model for Assessment of Carbon Sequestration in Grasslands of Kazakhstan: Combining Ground Biomass Data and Remote-sensing

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    A modified light use efficiency (LUE) model was tested in the grasslands of central Kazakhstan in terms of its ability to characterize spatial patterns and interannual dynamics of net primary production (NPP) at a regional scale. In this model, the LUE of the grassland biome (n) was simulated from ground-based NPP measurements, absorbed photosynthetically active radiation (APAR) and meteorological observations using a new empirical approach. Using coarse-resolution satellite data from the Sea-viewing Wide Field-of-view Sensor (SeaWiFS), monthly NPP was calculated from 1998 to 2008 over a large grassland region in Kazakhstan. The modelling results were verified against scaled up plot-level observations of grassland biomass and another available NPP data set derived from a field study in a similar grassland biome. The results indicated the reliability of productivity estimates produced by the model for regional monitoring of grassland NPP. The method for simulation of n suggested in this study can be used in grassland regions where no carbon flux measurements are accessible

    Response of CO<sub>2</sub> and H<sub>2</sub>O fluxes in a mountainous tropical rainforest in equatorial Indonesia to El NiΓ±o events

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    The possible impact of El NiΓ±o–Southern Oscillation (ENSO) events on the main components of CO<sub>2</sub> and H<sub>2</sub>O fluxes between the tropical rainforest and the atmosphere is investigated. The fluxes were continuously measured in an old-growth mountainous tropical rainforest in Central Sulawesi in Indonesia using the eddy covariance method for the period from January 2004 to June 2008. During this period, two episodes of El NiΓ±o and one episode of La NiΓ±a were observed. All these ENSO episodes had moderate intensity and were of the central Pacific type. The temporal variability analysis of the main meteorological parameters and components of CO<sub>2</sub> and H<sub>2</sub>O exchange showed a high sensitivity of evapotranspiration (ET) and gross primary production (GPP) of the tropical rainforest to meteorological variations caused by both El NiΓ±o and La NiΓ±a episodes. Incoming solar radiation is the main governing factor that is responsible for ET and GPP variability. Ecosystem respiration (RE) dynamics depend mainly on the air temperature changes and are almost insensitive to ENSO. Changes in precipitation due to moderate ENSO events did not have any notable effect on ET and GPP, mainly because of sufficient soil moisture conditions even in periods of an anomalous reduction in precipitation in the region

    Π‘ΠΈΠ½Ρ‚Π΅Π· ΠΈΠ·Π»ΡƒΡ‡Π°ΡŽΡ‰Π΅ΠΉ систСмы, Ρ„ΠΎΡ€ΠΌΠΈΡ€ΡƒΡŽΡ‰Π΅ΠΉ ΡΠ΅ΠΊΡ‚ΠΎΡ€Π½ΡƒΡŽ Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡƒ направлСнности с ΠΌΠΈΠ½ΠΈΠΌΠΈΠ·Π°Ρ†ΠΈΠ΅ΠΉ эффСкта Гиббса

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    For the synthesis of radiating systems, which form the flat-topped radiation patterns there are some of the most convenient methods, including Fourier method, method of partial diagram and method of changing projections. These methods are handy for calculation, because they allow us to obtain the flat-topped radiation patterns with predetermined electrical characteristics. These are the following characteristics: side-lobe level, width of the main lobe of the radiation pattern, and amplitude of top ripple of the main lobe of the radiation pattern. Meeting the challenge of synthesizing flat-topped radiation pattern is complicated by the break points available in a predetermined radiation pattern, which prevent the convergence of the Fourier series. The points of discontinuity, in turn, lead to the emergence of extremes that are associated with the Gibb’s phenomenon. To eliminate them, are used different methods for approximating a given radiation pattern (a series of Kotelnikov polynomial and that of Chebyshev). Such approximation, in turn, imposes restrictions on the basic quality indicators the flat-topped radiation patterns, such as the steepness of fronts and top ripple of the main lobe of the radiation pattern. The proposed method provides the lowest side-lobe level with small amplitude of top ripple of the main lobe of the flat-topped radiation pattern. The paper offers a linear approximation option of the given radiation pattern, which allows a synthesized radiation pattern with a diversity of quality parameters. This is achieved by linear approximation coefficients that can be determined using optimization algorithms. Depending on the target function for the optimization algorithm it is possible to determine the best trade-off between making the steepness parameter of the fronts and the top ripple amplitude of the main lobe of the flat-topped radiation pattern. The important feature of the method is that it minimizes the Gibbs phenomenon and is easy to calculate gratings with the small number of radiators.Для синтСза ΠΈΠ·Π»ΡƒΡ‡Π°ΡŽΡ‰ΠΈΡ… систСм, Ρ„ΠΎΡ€ΠΌΠΈΡ€ΡƒΡŽΡ‰ΠΈΡ… сСкторныС Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности, ΡΡƒΡ‰Π΅ΡΡ‚Π²ΡƒΡŽΡ‚ нСсколько Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΡƒΠ΄ΠΎΠ±Π½Ρ‹Ρ… ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠ², срСди ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Ρ…: ΠΌΠ΅Ρ‚ΠΎΠ΄ Π€ΡƒΡ€ΡŒΠ΅, ΠΌΠ΅Ρ‚ΠΎΠ΄ ΠΏΠ°Ρ€Ρ†ΠΈΠ°Π»ΡŒΠ½Ρ‹Ρ… Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌ ΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄ ΠΈΠ·ΠΌΠ΅Π½ΡΡŽΡ‰ΠΈΡ…ΡΡ ΠΏΡ€ΠΎΠ΅ΠΊΡ†ΠΈΠΉ. Π”Π°Π½Π½Ρ‹Π΅ ΠΌΠ΅Ρ‚ΠΎΠ΄Ρ‹ ΡƒΠ΄ΠΎΠ±Π½Ρ‹ для расчСта, ΠΏΠΎΡ‚ΠΎΠΌΡƒ Ρ‡Ρ‚ΠΎ ΠΏΠΎΠ·Π²ΠΎΠ»ΡΡŽΡ‚ ΠΏΠΎΠ»ΡƒΡ‡ΠΈΡ‚ΡŒ сСкторныС Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности с Π·Π°Π΄Π°Π½Π½Ρ‹ΠΌΠΈ элСктричСскими характСристиками. Π­Ρ‚ΠΈΠΌΠΈ характСристиками ΡΠ²Π»ΡΡŽΡ‚ΡΡ: ΡƒΡ€ΠΎΠ²Π΅Π½ΡŒ Π±ΠΎΠΊΠΎΠ²Ρ‹Ρ… лСпСстков, ΡˆΠΈΡ€ΠΈΠ½Π° Π³Π»Π°Π²Π½ΠΎΠ³ΠΎ лСпСстка Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности ΠΈ Π°ΠΌΠΏΠ»ΠΈΡ‚ΡƒΠ΄Π° ΠΏΠ΅Ρ€Π΅ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ Π²Π΅Ρ€ΡˆΠΈΠ½Ρ‹ Π³Π»Π°Π²Π½ΠΎΠ³ΠΎ лСпСстка сСкторной Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности.Β Β  РСшСниС Π·Π°Π΄Π°Ρ‡ΠΈ синтСза сСкторной Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности ослоТняСтся Π½Π°Π»ΠΈΡ‡ΠΈΠ΅ΠΌ Ρ‚ΠΎΡ‡Π΅ΠΊ Ρ€Π°Π·Ρ€Ρ‹Π²Π° Π² Π·Π°Π΄Π°Π½Π½ΠΎΠΉ Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΠ΅ направлСнности, ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Π΅ ΠΏΡ€Π΅ΠΏΡΡ‚ΡΡ‚Π²ΡƒΡŽΡ‚ сходимости ряда Π€ΡƒΡ€ΡŒΠ΅. Π’ΠΎΡ‡ΠΊΠΈ Ρ€Π°Π·Ρ€Ρ‹Π²Π°, Π² свою ΠΎΡ‡Π΅Ρ€Π΅Π΄ΡŒ, приводят ΠΊ возникновСнию экстрСмумов, ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Π΅ связаны с эффСктом Гиббса. Для ΠΈΡ… устранСния ΠΏΡ€ΠΈΠΌΠ΅Π½ΡΡŽΡ‚ Ρ€Π°Π·Π»ΠΈΡ‡Π½Ρ‹Π΅ ΠΌΠ΅Ρ‚ΠΎΠ΄Ρ‹ аппроксимации Π·Π°Π΄Π°Π½Π½ΠΎΠΉ Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности (ΠΏΠΎΠ»ΠΈΠ½ΠΎΠΌΠ°ΠΌΠΈ рядов ΠšΠΎΡ‚Π΅Π»ΡŒΠ½ΠΈΠΊΠΎΠ²Π°, Π§Π΅Π±Ρ‹ΡˆΠ΅Π²Π°). ΠŸΠΎΠ΄ΠΎΠ±Π½Ρ‹Π΅ аппроксимации Π½Π°ΠΊΠ»Π°Π΄Ρ‹Π²Π°ΡŽΡ‚ ограничСния Π½Π° основныС качСствСнныС ΠΏΠΎΠΊΠ°Π·Π°Ρ‚Π΅Π»ΠΈ сСкторных Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌ направлСнности, Ρ‚Π°ΠΊΠΈΠ΅ ΠΊΠ°ΠΊ: ΠΊΡ€ΡƒΡ‚ΠΈΠ·Π½Ρƒ Ρ„Ρ€ΠΎΠ½Ρ‚ΠΎΠ² ΠΈ пСрСколСбания Π²Π΅Ρ€ΡˆΠΈΠ½Ρ‹ Π³Π»Π°Π²Π½ΠΎΠ³ΠΎ лСпСстка Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности. ΠŸΡ€Π΅Π΄Π»ΠΎΠΆΠ΅Π½Π½Ρ‹ΠΉ ΠΌΠ΅Ρ‚ΠΎΠ΄ позволяСт ΠΏΠΎΠ»ΡƒΡ‡ΠΈΡ‚ΡŒ наимСньший ΡƒΡ€ΠΎΠ²Π΅Π½ΡŒ Π±ΠΎΠΊΠΎΠ²Ρ‹Ρ… лСпСстков ΠΏΡ€ΠΈ Π½Π΅Π·Π½Π°Ρ‡ΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎΠΌ ΠΏΠ΅Ρ€Π΅ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΈ плоской Π²Π΅Ρ€ΡˆΠΈΠ½Ρ‹ Π³Π»Π°Π²Π½ΠΎΠ³ΠΎ лСпСстка сСкторной Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности. ΠŸΡ€Π΅Π΄Π»ΠΎΠΆΠ΅Π½ Π²Π°Ρ€ΠΈΠ°Π½Ρ‚ Π»ΠΈΠ½Π΅ΠΉΠ½ΠΎΠΉ аппроксимации Π·Π°Π΄Π°Π½Π½ΠΎΠΉ Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности, ΠΊΠΎΡ‚ΠΎΡ€Ρ‹ΠΉ позволяСт ΠΏΠΎΠ»ΡƒΡ‡Π°Ρ‚ΡŒ синтСзированныС Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности с Ρ€Π°Π·Π½ΠΎΠ³ΠΎ Ρ€ΠΎΠ΄Π° ΠΏΠ°Ρ€Π°ΠΌΠ΅Ρ‚Ρ€Π°ΠΌΠΈ качСства. Π­Ρ‚ΠΎ достигаСтся с ΠΏΠΎΠΌΠΎΡ‰ΡŒΡŽ коэффициСнтов Π»ΠΈΠ½Π΅ΠΉΠ½ΠΎΠΉ аппроксимации, ΠΊΠΎΡ‚ΠΎΡ€Ρ‹Π΅ ΠΌΠΎΠ³ΡƒΡ‚ Π±Ρ‹Ρ‚ΡŒ ΠΎΠΏΡ€Π΅Π΄Π΅Π»Π΅Π½Ρ‹ с ΠΏΠΎΠΌΠΎΡ‰ΡŒΡŽ Π°Π»Π³ΠΎΡ€ΠΈΡ‚ΠΌΠΎΠ² ΠΎΠΏΡ‚ΠΈΠΌΠΈΠ·Π°Ρ†ΠΈΠΈ. Π’ зависимости ΠΎΡ‚ Π²Ρ‹Π±Ρ€Π°Π½Π½ΠΎΠΉ Ρ†Π΅Π»Π΅Π²ΠΎΠΉ Ρ„ΡƒΠ½ΠΊΡ†ΠΈΠΈ для Π°Π»Π³ΠΎΡ€ΠΈΡ‚ΠΌΠ° ΠΎΠΏΡ‚ΠΈΠΌΠΈΠ·Π°Ρ†ΠΈΠΈ появляСтся Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΠΎΡΡ‚ΡŒ опрСдСлСния Π½Π°ΠΈΠ»ΡƒΡ‡ΡˆΠΈΡ… Ρ€Π΅ΡˆΠ΅Π½ΠΈΠΉ компромисса ΠΌΠ΅ΠΆΠ΄Ρƒ ΠΏΠ°Ρ€Π°ΠΌΠ΅Ρ‚Ρ€ΠΎΠΌ ΠΊΡ€ΡƒΡ‚ΠΈΠ·Π½Ρ‹ Ρ„Ρ€ΠΎΠ½Ρ‚ΠΎΠ² ΠΈ Π°ΠΌΠΏΠ»ΠΈΡ‚ΡƒΠ΄ΠΎΠΉ ΠΏΠ΅Ρ€Π΅ΠΊΠΎΠ»Π΅Π±Π°Π½ΠΈΠΉ Π²Π΅Ρ€ΡˆΠΈΠ½Ρ‹ Π³Π»Π°Π²Π½ΠΎΠ³ΠΎ лСпСстка сСкторной Π΄ΠΈΠ°Π³Ρ€Π°ΠΌΠΌΡ‹ направлСнности. Π’Π°ΠΆΠ½Ρ‹ΠΌΠΈ особСнностями Π΄Π°Π½Π½ΠΎΠ³ΠΎ ΠΌΠ΅Ρ‚ΠΎΠ΄Π° являСтся Ρ‚ΠΎ, Ρ‡Ρ‚ΠΎ ΠΎΠ½ позволяСт ΠΌΠΈΠ½ΠΈΠΌΠΈΠ·ΠΈΡ€ΠΎΠ²Π°Ρ‚ΡŒ эффСкт Гиббса ΠΈ ΡƒΠ΄ΠΎΠ±Π΅Π½ для расчСта Ρ€Π΅ΡˆΠ΅Ρ‚ΠΎΠΊ с ΠΌΠ°Π»Ρ‹ΠΌ числом ΠΈΠ·Π»ΡƒΡ‡Π°Ρ‚Π΅Π»Π΅ΠΉ

    Improving land cover classification using input variables derived from a geographically weighted principal components analysis

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    This study demonstrates the use of a geographically weighted principal components analysis (GWPCA) of remote sensing imagery to improve land cover classification accuracy. A principal components analysis (PCA) is commonly applied in remote sensing but generates global, spatially-invariant results. GWPCA is a local adaptation of PCA that locally transforms the image data, and in doing so, can describe spatial change in the structure of the multi-band imagery, thus directly reflecting that many landscape processes are spatially heterogenic. In this research the GWPCA localised loadings of MODIS data are used as textural inputs, along with GWPCA localised ranked scores and the image bands themselves to three supervised classification algorithms. Using a reference data set for land cover to the west of Jakarta, Indonesia the classification procedure was assessed via training and validation data splits of 80/20, repeated 100 times. For each classification algorithm, the inclusion of the GWPCA loadings data was found to significantly improve classification accuracy. Further, but more moderate improvements in accuracy were found by additionally including GWPCA ranked scores as textural inputs, data that provide information on spatial anomalies in the imagery. The critical importance of considering both spatial structure and spatial anomalies of the imagery in the classification is discussed, together with the transferability of the new method to other studies. Research topics for method refinement are also suggested

    The use of NDVI and its Derivatives for Monitoring Lake Victoria’s Water Level and Drought Conditions

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    Normalized Difference Vegetation Index (NDVI), which is a measure of vegetation vigour, and lake water levels respond variably to precipitation and its deficiency. For a given lake catchment, NDVI may have the ability to depict localized natural variability in water levels in response to weather patterns. This information may be used to decipher natural from unnatural variations of a given lake’s surface. This study evaluates the potential of using NDVI and its associated derivatives (VCI (vegetation condition index), SVI (standardised vegetation index), AINDVI (annually integrated NDVI), green vegetation function (F g ), and NDVIA (NDVI anomaly)) to depict Lake Victoria’s water levels. Thirty years of monthly mean water levels and a portion of the Global Inventory Modelling and Mapping Studies (GIMMS) AVHRR (Advanced Very High Resolution Radiometer) NDVI datasets were used. Their aggregate data structures and temporal co-variabilities were analysed using GIS/spatial analysis tools. Locally, NDVI was found to be more sensitive to drought (i.e., responded more strongly to reduced precipitation) than to water levels. It showed a good ability to depict water levels one-month in advance, especially in moderate to low precipitation years. SVI and SWL (standardized water levels) used in association with AINDVI and AMWLA (annual mean water levels anomaly) readily identified high precipitation years, which are also when NDVI has a low ability to depict water levels. NDVI also appears to be able to highlight unnatural variations in water levels. We propose an iterative approach for the better use of NDVI, which may be useful in developing an early warning mechanisms for the management of lake Victoria and other Lakes with similar characteristics
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