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Remote temperature sensing at the micro‐ and nanoscale is key in fields such as photonics, electronics, energy, or biomedicine, with optical properties being one of the most used transducing mechanisms for such sensors. Ga2O3 presents very high chemical and thermal stability, as well as high radiation resistance, becoming of great interest to be used under extreme conditions, for example, electrical and/or optical high‐power devices and harsh environments. In this work, a luminescent and interferometric thermometer is proposed based on Fabry–Perot (FP) optical microcavities built on Cr‐doped Ga2O3 nanowires. It combines the optical features of the Cr3+‐related luminescence, greatly sensitive to temperature, and spatial confinement of light, which results in strong FP resonances within the Cr3+ broad band. While the chromium‐related R lines energy shifts are adequate for low‐temperature sensing, FP resonances extend the sensing range to high temperatures with excellent sensitivity. This thermometry system achieves micron‐range spatial resolution, temperature precision of around 1 K, and a wide operational range, demonstrating to work at least in the 150–550 K temperature range. Besides, the temperature‐dependent anisotropic refractive index and thermo‐optic coefficient of this oxide have been further characterized by comparison to experimental, analytical, and finite‐difference time‐domain simulation results.

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SUMMARY Tenerife is one of the most well monitored islands of the Canaries, but the surveillance generally is centred on Las Cañadas Caldera, where the Teide volcano is located. In the last 180 000 yr, the eruptions on Tenerife Island have never occurred in the same volcanic structure, except for the Teide and Pico Viejo central volcanic system, so that a complete monitoring network would have to cover the whole island. As a result, Synthetic Aperture Radar Interferometry (InSAR) is being used on Tenerife, because this space technique can provide a displacement map of the surface of the earth with centimetre precision. This paper presents the results obtained on Tenerife Island using 18 SAR images acquired by the ERS‐1 and ERS‐2 satellites during the period 1992–2000. Two important results have been obtained: no deformation on Las Cañadas Caldera, coinciding with results obtained using terrestrial techniques, and two subsidence episodes outside monitoring areas in the NW of the island, in the region of the last historic eruptions. These results show that InSAR is a useful technique for monitoring the entire island, thus allowing us to discover deformations in areas that are not routinely or easily monitored. This technique has been used in combination with Global Positioning System (GPS) observation of a global network on the island to define a new geodetic monitoring system. The possible causes of the deformations observed have been studied in an endeavour to discern if they might be of natural origin, in particular linked to a reactivation of prior volcanic activity. Examination of the geophysical observations on the island, human activities underway and the results of the modelling seem to indicate that at least part of the deformations may be caused by changes in the groundwater level and therefore are not linked to a volcanic reactivation. This result is important because it implies that, if geodetic volcano monitoring is to be performed on the island, the system used must be capable of discerning between various possible origins of the deformation by analysing their patterns and ancillary information from other sources. In this regard, InSAR is a basic tool on account of its unpaired wide area coverage and spatial density.

There was significant eruptive activity on Lanzarote (Canary Islands) in the 18th and 19th centuries, and future activity is a clear likelihood today. The fact that not all of the island is covered by geodetic monitoring prompted the authors to assess the possibility of using SAR interferometry for routine volcanic activity monitoring of the island. This paper presents the results obtained after testing this technique using six radar images acquired by the ERS-1 and ERS-2 satellites during the period 1992-2000. The analysis of these images has confirmed the existence of long-term stability coherence across most of the island: a prerequisite for using SAR interferometry in volcano monitoring. The analysis of 15 (redundant) interferograms allowed us to study both the impact of atmospheric artifacts on Lanzarote and any possible displacements, and to conclude that there has been no displacement greater than 3 cm on the island during the period in question. This result matches those obtained with the geodetic equipment installed on the island. Our results show that the inclusion of SAR interferometry in routine geodetic monitoring, supplementing terrestrial techniques, will clearly improve the chances of detecting any possible deformation, and its broad coverage will enhance the interpretation of any observed anomalies.