Fig. 5From: Effusive crises at Piton de la Fournaise 2014–2015: a review of a multi-national response model a MIROVA-derived TADRs (circles) recorded during the May 2015 eruption. Uncertainty related to variable emplacement styles or underlying topography is taken into account by the upper and lower bounds of each TADR estimate (thin solid lines). b Example of thermal image (Brightness Temperature at 3.9 μm: MODIS band 22) output by the MIROVA system and overlain (in transparency) on Google Earth to allow rapid geolocation of thermally anomalous pixelsBack to article page