Emissivity-based vegetation indices to monitor deforestation and forest degradation in the Congo basin rainforest

Vegetation stress is a major widespread problem in many countries because of climate change and anthropogenic activities. Deforestation and forest degradation phenomena may be caused for several reasons such as infrastructure development, agriculture, collection of wood energy, forest exploitation. Over the last decade, a severe decline in vegetation was observed in the Congo Basin rainforest, the second-largest tropical forest in the world, behind the Amazon. Therefore, actions are required to monitor and detect vegetation stresses to mitigate their negative impacts on human life, wildlife, and plant communities. Vegetation stress can be estimated using three different methods: field measurements, meteorological data, and remote sensing. The present study is mainly focused on satellite remote sensing. The main objective is to develop and test new indices of vegetation-soil dryness based on the surface emissivity. Until now, the problem has been attacked through indices such as the normalized differential vegetation index (or NDVI). The problem of NDVI is that it is a greenness index and is not capable to distinguish bare soil from senescent vegetation, whereas this distinction is important especially when forest degradation followed by eventual regeneration occurs and when dealing with semi-arid regions, where we could have desert sand. We propose to follow the strategy of using surface emissivity (ε), which is more closely related to surface type and coverage. By properly using surface emissivity in the infrared we can define a set of channels that are particularly sensitive to bare soil, green, and senescent vegetation. From these emissivity channels, we can derive a suitable emissivity contrast index or ECI, which is sensitive to green vegetation, senescent vegetation, and bare soil, therefore overcoming the NDVI limitation concerning its capability to distinguish bares soil from senescent vegetation. The analysis is performed with CAMEL (Combined ASTER and MODIS Emissivity for Land) database from 2000 to 2016.

[1]  Xavier Ceamanos,et al.  Can We Detect the Brownness or Greenness of the Congo Rainforest Using Satellite-Derived Surface Albedo? A Study on the Role of Aerosol Uncertainties , 2019, Sustainability.

[2]  I. D. Feis,et al.  Kalman filter physical retrieval of surface emissivity and temperature from geostationary infrared radiances , 2013 .

[3]  P. Ciais,et al.  Widespread decline of Congo rainforest greenness in the past decade , 2014, Nature.

[4]  L. Mubalama,et al.  Monitoring law enforcement and illegal activities in the northern sector of the Parc National des Virunga, Democratic Republic of Congo , 2004 .

[5]  Offer Rozenstein,et al.  Diurnal emissivity dynamics in bare versus biocrusted sand dunes. , 2015, The Science of the total environment.

[6]  T. Tadesse,et al.  The Vegetation Drought Response Index (VegDRI): A New Integrated Approach for Monitoring Drought Stress in Vegetation , 2008 .

[7]  Laurent Poutier,et al.  SEVIRI Hyper-Fast Forward Model with Application to Emissivity Retrieval , 2019, Sensors.

[8]  C. Serio,et al.  Hyper fast radiative transfer for the physical retrieval of surface parameters from SEVIRI observations , 2015 .

[9]  Simon J. Hook,et al.  The Combined ASTER MODIS Emissivity over Land (CAMEL) Part 1: Methodology and High Spectral Resolution Application , 2018, Remote. Sens..

[10]  Jean‐François Bastin,et al.  Using fragmentation to assess degradation of forest edges in Democratic Republic of Congo , 2016, Carbon Balance and Management.

[11]  I. F. Trigo,et al.  Kalman filter physical retrieval of surface emissivity and temperature from SEVIRI infrared channels: a validation and intercomparison study , 2015 .

[12]  Eva Borbas,et al.  Diurnal variation in Sahara desert sand emissivity during the dry season from IASI observations , 2014 .

[13]  C. Tucker,et al.  North American vegetation patterns observed with the NOAA-7 advanced very high resolution radiometer , 1985, Vegetatio.

[14]  Laurent Poutier,et al.  Physical Retrieval of Land Surface Emissivity Spectra from Hyper-Spectral Infrared Observations and Validation with In Situ Measurements , 2018, Remote. Sens..

[15]  T. Schmugge,et al.  Discrimination of Senescent Vegetation Using Thermal Emissivity Contrast , 2000 .

[16]  Peter J. Rousseeuw,et al.  Finding Groups in Data: An Introduction to Cluster Analysis , 1990 .

[17]  Eva Borbas,et al.  The Combined ASTER MODIS Emissivity over Land (CAMEL) Part 2: Uncertainty and Validation , 2018, Remote. Sens..

[18]  Jesslyn F. Brown,et al.  Measuring phenological variability from satellite imagery , 1994 .

[19]  J. Malingreau Global vegetation dynamics - Satellite observations over Asia , 1986 .

[20]  Michele Brunetti,et al.  The impact of drought spells on forests depends on site conditions: The case of 2017 summer heat wave in southern Europe , 2019, Global change biology.

[22]  S. P. Lloyd,et al.  Least squares quantization in PCM , 1982, IEEE Trans. Inf. Theory.

[23]  Thomas R. Loveland,et al.  An approach for using AVHRR data to monitor U.S. Great Plains Grasslands , 1996 .

[24]  Sara Venafra,et al.  Surface parameters from seviri observations through a kalman filter approach: Application and evaluation of the scheme to the southern Italy , 2016 .

[25]  Sergei Vassilvitskii,et al.  k-means++: the advantages of careful seeding , 2007, SODA '07.