Diseño e implementación de un espectrómetro y un polarímetro para la diagnosis de plasmas de aire producidos por eventos luminosos transitorios en la mesofera terrestre
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Passas Varo, MaríaEditorial
Universidad de Granada
Departamento
Universidad de Granada. Programa Oficial de Doctorado en: Física y Ciencias del Espacio; Consejo Superior de Investigaciones Científicas (CSIC). Instituto de Astrofísica de AndalucíaMateria
Polarimetría Espectrómetros Polarización (Luz) Espectros Plasmas cósmicos Transient Luminous Events (TLEs) Granada Sprite Spectograph and Polarimeter (GRASSP) Luminiscencia
Materia UDC
521.1 21
Date
2017Fecha lectura
2017-06-19Referencia bibliográfica
Passas Varo, M. Diseño e implementación de un espectrómetro y un polarímetro para la diagnosis de plasmas de aire producidos por eventos luminosos transitorios en la mesofera terrestre. Granada: Universidad de Granada, 2017. [http://hdl.handle.net/10481/47120]
Sponsorship
Tesis Univ. Granada. Programa Oficial de Doctorado en: Física y Ciencias del Espacio; This work has been made possible with the nancial assistance of the Spanish Ministry of Science and Innovation, MINECO (previously MICINN) under projects AYA2009-14027-C05-02, AYA2011-29936-546-C05-02, ESP2013- 48032-C5-5-R, FIS2014-61774-EXP, ESP2015-69909-C5-2-R and FQM{5965; the European Science Foundation (ESF) Research Networking Programmes under project 09-RNP-101 and the EU through the FEDER program.Abstract
In this work of thesis we thoroughly describe the design, development and
characterization of a new diagnosis instrument intended to perform systematic
campaigns of simultaneous measurement of the spectrum and polarization
degree of the light emitted by transient luminous events (TLEs) as a
ground support to space missions ASIM (ESA) and TARANIS (CNES) to
be launched by early and late 2018, respectively.
The GRASSP instrument (GRAnada Sprite Spectrograph and Polarimeter)
includes the first medium{high spectrograph specifically designed for
the analysis of air plasmas generated by TLEs. All versions of GRASSP
have been developed and characterized by our group at the Institute of
Astrophysics of Andalusia (IAA, Granada, Spain) and the Institute of Matter
Structure (IEM, Madrid, Spain) laboratories, both dependencies of the
National Research Council of Spain (CSIC).
We have developed four different versions of GRASSP to date. We installed
the first (2012 { 2014) and second (2014 { 2015) versions of GRASSP at
the Spanish{German Astronomic Center (CAHA) in Calar Alto, Almería,
Spain. Both worked in an autonomous way, without the support of an operator.
Every sunset, the system powered on automatically, took the calibration
images, opened the blinds of the system and aimed the spectrograph
to the region of the sky where a TLE was more probable to appear. This
could be done thanks to an aiming algorithm we developed that queried the
databases of the Spanish Weather Agency in real-time and calculated the
coordinates of the closest storm. When the system detected a change of the
brightness level in the sky, an audio trigger system launched the simultaneous
recording of both field image and spectral image to store them in a data
repository. This way we could discern the origin of the recorded spectra. Every sunrise, after the observation night, the algorithm closed blinds and
switched off all the GRASSP subsystems. From this location we obtained
the first TLE images recorded with GRASSP, we recorded several spectra
from lightning optical emissions dispersed on clouds and we had the chance
of recording a meteoroid spectrum while it passed in front of GRASSP.
Unfortunately, from this location we did not record any TLE spectra because
of the remoteness of the storms, that occur most frequently in Spain
in the Ebro Delta valley. Hence we decided to relocate our spectrograph
in a new and compact version of GRASSP. We installed GRASSP versions
three (2015 { 2016) and four (2016 { now) in Castellgallí, Barcelona, Spain.
This last compact version is currently located within the stormiest region
of north-eastern Spain, with a field of view of almost 360 degrees, and it
is manually aimed by an experienced colleague (Oscar Van der Velde, from
Polytechnic University of Catalonia). Since the installation of the third version
of GRASSP we have recorded up to 44 medium{high resolution TLE
spectra, that allowed us to quantify, for the first time, the (rotational) temperature
of gas surrounding TLEs. It can be done through the spectral fitting
of the recorded spectrum to synthetic spectrum that we have modelled,
thanks to the high resolution of our spectrograph (0.235 nm) that allows
us to fit the rovibrational bands of the nitrogen molecule. This way we
can understand TLEs as natural probes of the air temperature in the Earth
mesosphere. It is the first time that systematic campaigns of spectroscopic
measurements of TLEs with such high resolution have been developed (the
best spectral resolution to date intended to sporadically analyze TLEs spectra
is 3 nm), with the goal of feeding a database to statistically characterize
the TLEs from a spectroscopic point of view in a near future.
The GRASSP polarimeter is currently in calibration stage within our laboratories.
It is intended to be operative from summer 2017.