2016 ◽  
Vol 122 ◽  
pp. 222-235 ◽  
Author(s):  
Louis Gonzalez ◽  
François-Marie Bréon ◽  
Karine Caillault ◽  
Xavier Briottet

Author(s):  
Raffaella Matarrese ◽  
Nicolas Guyennon ◽  
Diego Copetti

In winter 2008-2009, Lake Occhito, a strategic multiple-uses reservoir in South Italy, was affected by an extraordinary Planktothrix rubescens bloom. P. rubescens is a filamentous potentially toxic cyanobacterium which has recently colonized many environments in Europe. A number of studies is currently available on the use of remote sensing techniques to monitor different fresh water cyanobacteria species. By contrast no specific applications are available on the remote sensing monitoring of P. rubescens. In this paper we present a specific algorithm, based on Water Leaving Reflectances (WLR) from MERIS data, atmospherically corrected using the Aerosol Optical Thickness (AOT) retrieved by MODIS data, to detect P. rubescens blooms. The high accuracy in AOT data, provided by MOD09 surface reflectance product, at 1km spatial resolution, allowed obtaining a good correlation between the WLR and the P. rubescens chlorophyll-a concentrations measured in the field, through multiple stations fluorometric profiles. A modified Normalized Difference Chlorophyll index (NDCI) algorithm is presented. The performance of the proposed algorithm has been successfully compared with other specific algorithms for turbid productive waters. We demonstrated how important is to verify the spectral behaviour of bio-optical parameters in order to develop an ad hoc algorithm that better performs with respect to standard algorithms.


2017 ◽  
Author(s):  
Kimberly A. Casey ◽  
Chris M. Polashenski ◽  
Justin Chen ◽  
Marco Tedesco

Abstract. We evaluate Greenland Ice Sheet (GrIS) surface reflectance and albedo trends using the newly released Collection 6 (C6) MODIS products over the period 2001–2016. We find that the correction of MODIS sensor degradation provided in the new C6 data products reduces the magnitude of the surface reflectance and albedo decline trends obtained from previous MODIS data (i.e. Collection 5, C5). Collection 5 and 6 data product analysis over GrIS is characterized by surface (i.e. wet vs. dry) and elevation (i.e. 500 m–2000 m, 2000 m and greater) conditions over the summer season from June 1–August 31. Notably, the visible-wavelength declining reflectance trends identified in several bands MODIS C5 data from previous studies are only slightly detected, at reduced magnitude in the C6 versions over the dry snow zone. Wet snow albedo decline over the MODIS record remains in the C6 product, albeit at a lower magnitude than obtained using C5 data. Further analysis of C6 spectral reflectance trends show both reflectance increases and decreases in select bands and regions, suggesting that several competing processes are contributing to ice sheet albedo change. Investigators using MODIS data in other fields may consider similar re-examinations of trends previously established using C5 data.


2012 ◽  
Vol 38 (1) ◽  
pp. 9-22 ◽  
Author(s):  
Min Feng ◽  
Chengquan Huang ◽  
Saurabh Channan ◽  
Eric F. Vermote ◽  
Jeffrey G. Masek ◽  
...  

2017 ◽  
Vol 11 (4) ◽  
pp. 1781-1795 ◽  
Author(s):  
Kimberly A. Casey ◽  
Chris M. Polashenski ◽  
Justin Chen ◽  
Marco Tedesco

Abstract. We evaluate Greenland Ice Sheet (GrIS) surface reflectance and albedo trends using the newly released Collection 6 (C6) MODIS (Moderate Resolution Imaging Spectroradiometer) products over the period 2001–2016. We find that the correction of MODIS sensor degradation provided in the new C6 data products reduces the magnitude of the surface reflectance and albedo decline trends obtained from previous MODIS data (i.e., Collection 5, C5). Collection 5 and 6 data product analysis over GrIS is characterized by surface (i.e., wet vs. dry) and elevation (i.e., 500–2000 m, 2000 m and greater) conditions over the summer season from 1 June to 31 August. Notably, the visible-wavelength declining reflectance trends identified in several bands of MODIS C5 data from previous studies are only slightly detected at reduced magnitude in the C6 versions over the dry snow area. Declining albedo in the wet snow and ice area remains over the MODIS record in the C6 product, albeit at a lower magnitude than obtained using C5 data. Further analyses of C6 spectral reflectance trends show both reflectance increases and decreases in select bands and regions, suggesting that several competing processes are contributing to Greenland Ice Sheet albedo change. Investigators using MODIS data for other ocean, atmosphere and/or land analyses are urged to consider similar re-examinations of trends previously established using C5 data.


2006 ◽  
Author(s):  
Wang Ying ◽  
Yong Xue ◽  
Jianping Guo ◽  
Yincui Hu ◽  
Ying Luo ◽  
...  

2002 ◽  
Vol 83 (1-2) ◽  
pp. 97-111 ◽  
Author(s):  
Eric F Vermote ◽  
Nazmi Z El Saleous ◽  
Christopher O Justice

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