Mediterranean forests are every year affected by wildfires which have a significant effect on the ecosystem. Mapping
burned areas is an important field of application for optical remote sensing techniques and several methodologies have
been developed in order to improve mapping accuracy. We developed an automated procedure based on spectral indices
and fuzzy theory for mapping burned areas from atmospherically corrected Landsat TM images. The algorithm proved to
provide consistent accuracy over Mediterranean areas. We further tested algorithm’s performance to assess the influence
of the atmospheric correction on the accuracy of burned areas. In particular, we ran the Second Simulation of a Satellite
Signal in the Solar Spectrum (6S) code with different Atmospheric Optical Thickness (AOT) levels and two aerosol
models (continental and maritime) on one TM image acquired over Portugal (12/08/2003). Burned area maps derived
from atmospherically corrected images and from the non corrected image (Top Of Atmosphere, TOA) have been
analyzed. In the output burned areas maps the omission error varies in the range 4.6-6.5% and the commission error
fluctuates between 11.9 and 22.2%; the highest omission (commission) errors occur with the continental (maritime)
model. The accuracy of burned area maps derived from non corrected image is very low, with omission error greater than
90%. These results show that, although atmospheric correction is needed for the application of the algorithm, the AOT
value does not significantly affect the performance.
Large wildfires in forests of southern European countries such as Portugal, Spain, Greece, France and Italy are one key
ecological disturbance of the Mediterranean environment. Optical data have been largely used for burned area mapping and literature provides an extensive reference for the typical spectral signal of burns and the methodologies applied to extract burn perimeters. However, optical remote sensing techniques have the major limitation of a reduced frequency of clear images due to cloud cover; moreover, for the specific application of burned area mapping, unburned targets such as shadows, can be spectrally confused and misclassified as burns. For this reason radar images could be integrated as an additional source of information. We developed an approach for mapping burned areas in Mediterranean regions based on Landsat TM/ETM+ data and vegetation indices that provided satisfactory results. However, we are currently working for further improving our approach by exploiting the synergy between optical and radar data. In this paper we present the first results of the analysis of the SAR backscatter over burned areas for future integration into the formal framework previously developed. Although results are preliminary, they encourage us to test the approach over different regions of the Mediterranean environment to evaluate its robustness.
Leaf area index (LAI) is a key variable for modeling the interaction between vegetation and the atmosphere. We collected field LAI measurements over 12 sites in 2005 in the Lys valley, Northern Italy, to calibrate regressive models using normalized difference vegetation index (NDVI), enhanced vegetation index (EVI), and wide dynamic range vegetation index (WDRVI) products derived from 250-m moderate resolution imaging spectroradiomete (MODIS) imagery. Field data were compared to the 1 km MODIS leaf area index-fraction of photosynthetically active radiation (LAI/fAPAR) product to show that regressive techniques are better suited for local applications. We investigated these LAI-vegetation index (VI) regressive models to 1. test the sensitivity of the model to forest type and phenology, 2. identify the most suitable VI for LAI retrieval, and 3. verify the feasibility of using a linear model. Results show that in our experimental conditions the LAI-VI relationship is primarily influenced by phenology and that the leaf constant period (maximum LAI) is significantly different compared to the other phenological phases. Among the indices, EVI yielded the poorest performance (R2<0.41) and the linear regressive models for NDVI and WDRVI derived by pooling together data from different phenological phases show a good correlation with field data (R2>0.65); the use of a logarithmic model does not improve the performance. The LAI-WDRVI and LAI-NDVI models were inverted and applied to 2004 MODIS data and model performance was assessed by comparing predicted and measured LAI. Results show that WDRVI performs best in a linear regressive model, yielding a relative root mean square error <23%.
The Sahelian belt of West Africa is a region characterized by wide climate variations, which can in turn affect the
survival of local populations especially in rangeland, as happened during the dramatic food crisis in the 70-80s caused by
severe drought. This work has been carried out in the framework of the EU FP7 Geoland2 project as a contribution to the
ECOWAS component (Economic Community Of West African States) of the AMESD (African Monitoring of the
Environment for Sustainable Development) programme with the purpose of establishing the reliability of Dry Matter
Productivity (DMP) developed by Flemish Institute for Technological Research (VITO), a spatial estimation of dry
matter (DM) obtained from remotely sensed data. DMP can be of great help in monitoring savanna pasturelands in a
region characterized by food insecurity and a significant variability of biomass production, linked to climate variations,
which can in turn affect the survival of local populations. The evaluation of DMP was carried out thanks to the Centre de
Suivi Ecologique (CSE) and Action Contre la Fame (ACF), the partners who provided the field biomass measurements.
The paper shows the correlation of DMP with field measurements of herbaceous biomass, and discusses the differences
among the different sites where ground data were collected. The analysis of other environmental variables (land cover,
rainfall), which can be influential on rangeland biomass production, is presented in order to better explain the variance of
field measurements among the different years.
Natural Resource Monitoring in Africa (NARMA) is one of the Core Information Services of EU-FP7 project Geoland2
addressing important sectoral policies that concern with the development of an environmental monitoring capacity over
African countries for the needs of the European Commission (EC) services and for regional and continental EC partners
in African countries. Congo basin is one of the target area where NARMA has to contribute to the development of
AMESD/CICOS services in support to management of water resources focusing on environmental aspects of watersheds.
In this contest and to better understand dynamics that occur in the watershed, an analysis has been conducted on the
relation between precipitation, river discharge and vegetation dynamics by exploiting available time series of Earth
Observation data. Rainfall dynamics has been described using FEWS-NET RFE estimations, river discharge has been
monitored using ENVISAT radar altimeter data provided by LEGOS laboratory and vegetation dynamics have been
examined through vegetation indices available from long term series of SPOT-VGT data. The comparison between river
discharge measured at Bangui (Central African Republic), gauging station and radar altimeter virtual station data
demonstrated that these data can be used to estimate river discharge. This result allowed to focus a preliminary analysis
on the Uele watershed, Ubangi sub basin, using radar data as a proxy of river discharge, comparing these trends to
seasonal rainfall estimates and trying to disentangling the effect of vegetation on discharge-rain relation. Results showed
that a strong positive correlation is obtained between rain data and river discharge only at the end of the vegetation
season when plants have reduced water demand for evapotranspiration and less intercept rain. Trend analysis on the
considered time windows are provided and the contribution of these finding for river water alert monitoring system is discussed.
Monitoring crop conditions and assessing nutrition requirements is fundamental for implementing sustainable agriculture. Rational nitrogen fertilization is of particular importance in rice crops in order to guarantee high production levels while minimising the impact on the environment. In fact, the typical flooded condition of rice fields can be a significant source of greenhouse gasses. Information on plant nitrogen concentration can be used, coupled with information about the phenological stage, to plan strategies for a rational and spatially differentiated fertilization schedule. A field experiment was carried out in a rice field Northern Italy, in order to evaluate the potential of field radiometric measurements for the prediction of rice nitrogen concentration. The results indicate that rice reflectance is influenced by nitrogen supply at certain wavelengths although N concentration cannot be accurately predicted based on the reflectance measured at a given wavelength. Regression analysis highlighted that the visible region of the spectrum is most sensitive to plant nitrogen concentration when reflectance measures are combined into a spectral index. An automated procedure allowed the analysis of all the possible combinations into a Normalized Difference Index (NDI) of the narrow spectral bands derived by spectral resampling of field measurements. The derived index appeared to be least influenced by plant biomass and Leaf Area Index (LAI) providing a useful approach to detect rice nutritional status. The validation of the regressive model showed that the model is able to predict rice N concentration (R2=0.55 [p<0.01]; RRMSE=29.4; modelling efficiency close to the optimum value).
Crop growth and production can be simulated by models for the whole canopy as a function of intercepted radiation, water availability, air temperature and nitrogen availability. Simulation models supply quantitative outputs starting from quantitative inputs and they need quite complex databases to run simulations. In practice, the more complex and physically based these tools are, the more inputs are required for their application. In most cases such data are not available. This is the reason why, for large scale evaluations, simplified models are often applied and satellite data are used as input. In particular, multi-temporal Earth Observation data represent a valid tool to define crop phenological stages and derive temporal and spatial variability of vegetation biophysical parameters, such as the Leaf Area Index (LAI). In 2003 and 2004 two intensive field campaigns were conducted over different areas of the Italian Rice Belt, Northern Italy, with the objective of collecting data for growth model calibration. Field spectroradiometer measurements and LAI estimation, retrieved by LAI2000, have been used to study the best Vegetation Index (VI) for rice growth monitoring. VI vs LAI relationship has been scaled up to MODIS data to produce LAI map for the entire growing season and the key phenological rice events have been detected by multitemporal MODIS analysis. Preliminary results of rice production estimation using a Light Use efficiency model that ingests spatially distributed phenological information are presented. Comparison with CropSyst model phenological parameters are provided and the contribution of multi-temporal EO data for regional crop monitoring is discussed.
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