Zero-pressure balloons trajectory prediction: Duster flight simulations

DUSTER (Dust from the Upper Stratosphere Tracking Experiment and Retrieval) is a balloon-born instrument designed to collect dust particles with sizes less than 30 μm in the upper stratosphere (30 – 40 km), to be analysed in laboratory. In support to the DUSTER flight campaigns, it is crucial to pre...

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Published in:Advances in Space Research
Main Authors: Liuzzi V., Della Corte V., Rotundi A., Ivanovski S., Dionnet Z., Brunetto R., Inno L.
Other Authors: Liuzzi, V., Della Corte, V., Rotundi, A., Ivanovski, S., Dionnet, Z., Brunetto, R., Inno, L.
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/11367/86133
https://doi.org/10.1016/j.asr.2020.07.011
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author Liuzzi V.
Della Corte V.
Rotundi A.
Ivanovski S.
Dionnet Z.
Brunetto R.
Inno L.
author2 Liuzzi, V.
Della Corte, V.
Rotundi, A.
Ivanovski, S.
Dionnet, Z.
Brunetto, R.
Inno, L.
author_facet Liuzzi V.
Della Corte V.
Rotundi A.
Ivanovski S.
Dionnet Z.
Brunetto R.
Inno L.
author_sort Liuzzi V.
collection Università degli Studi di Napoli "Parthenope": CINECA IRIS
container_issue 8
container_start_page 1876
container_title Advances in Space Research
container_volume 66
description DUSTER (Dust from the Upper Stratosphere Tracking Experiment and Retrieval) is a balloon-born instrument designed to collect dust particles with sizes less than 30 μm in the upper stratosphere (30 – 40 km), to be analysed in laboratory. In support to the DUSTER flight campaigns, it is crucial to predict the balloon trajectories according to atmospheric circulation and to estimate the landing. For a feasibility study of an Antarctic flight campaign we predict the DUSTER trajectory with a statistical approach, considering safety issues and the pivotal instrument recovery, to retrieve the collected samples. To this aim, we used the NOAA (National Oceanic and Atmospheric Administration) meteorological data and the HYSPLIT software (HYbrid Single Particle Lagrangian Integrated Trajectory). The Antarctic Polar Vortex, every year in the period December – January, generates a counter clockwise circulation (averaged wind speeds around 36 m/s from 29 to 35 km of altitudes). We evaluated the best launch opportunity windows for DUSTER to take advantage of the Polar Vortex starting from historical data. The NOAA meteorological data (Global reanalysis of atmospheric data – GFS Analysis and Forecasts products of the National Centers for Environmental Predictions - NCEP) from 1994 to 2015 allowed us to select the period after the 10th of January as the launch window maximizing the DUSTER time of flight. We used HYSPLIT program to project the balloon simulated trajectories on ground, providing critical information for the recovery operations. Successively, with the aim of becoming autonomous within the DUSTER team, i.e. taking care of the complete procedure to realize a DUSTER flight campaign, we developed a dedicated software, the DUSTER Flight Simulation Predictor (DFSP) that considers the ascent, floating and descent phases and the meteorological conditions. DFSP considers the balloon dynamics, the heat flow transfer between the balloon and the atmosphere, and the lifting variable gas mass to simulate the complete flight. We ...
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spelling ftuninapoliparth:oai:ricerca.uniparthenope.it:11367/86133 2025-01-16T19:09:48+00:00 Zero-pressure balloons trajectory prediction: Duster flight simulations Liuzzi V. Della Corte V. Rotundi A. Ivanovski S. Dionnet Z. Brunetto R. Inno L. Liuzzi, V. Della Corte, V. Rotundi, A. Ivanovski, S. Dionnet, Z. Brunetto, R. Inno, L. 2020 http://hdl.handle.net/11367/86133 https://doi.org/10.1016/j.asr.2020.07.011 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000569563600005 volume:66 issue:8 firstpage:1876 lastpage:1886 numberofpages:11 journal:ADVANCES IN SPACE RESEARCH http://hdl.handle.net/11367/86133 doi:10.1016/j.asr.2020.07.011 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85088959266 DUSTER Flight Simulation Predictor Numerical simulation Zero–pressure balloons info:eu-repo/semantics/article 2020 ftuninapoliparth https://doi.org/10.1016/j.asr.2020.07.011 2024-03-21T18:03:02Z DUSTER (Dust from the Upper Stratosphere Tracking Experiment and Retrieval) is a balloon-born instrument designed to collect dust particles with sizes less than 30 μm in the upper stratosphere (30 – 40 km), to be analysed in laboratory. In support to the DUSTER flight campaigns, it is crucial to predict the balloon trajectories according to atmospheric circulation and to estimate the landing. For a feasibility study of an Antarctic flight campaign we predict the DUSTER trajectory with a statistical approach, considering safety issues and the pivotal instrument recovery, to retrieve the collected samples. To this aim, we used the NOAA (National Oceanic and Atmospheric Administration) meteorological data and the HYSPLIT software (HYbrid Single Particle Lagrangian Integrated Trajectory). The Antarctic Polar Vortex, every year in the period December – January, generates a counter clockwise circulation (averaged wind speeds around 36 m/s from 29 to 35 km of altitudes). We evaluated the best launch opportunity windows for DUSTER to take advantage of the Polar Vortex starting from historical data. The NOAA meteorological data (Global reanalysis of atmospheric data – GFS Analysis and Forecasts products of the National Centers for Environmental Predictions - NCEP) from 1994 to 2015 allowed us to select the period after the 10th of January as the launch window maximizing the DUSTER time of flight. We used HYSPLIT program to project the balloon simulated trajectories on ground, providing critical information for the recovery operations. Successively, with the aim of becoming autonomous within the DUSTER team, i.e. taking care of the complete procedure to realize a DUSTER flight campaign, we developed a dedicated software, the DUSTER Flight Simulation Predictor (DFSP) that considers the ascent, floating and descent phases and the meteorological conditions. DFSP considers the balloon dynamics, the heat flow transfer between the balloon and the atmosphere, and the lifting variable gas mass to simulate the complete flight. We ... Article in Journal/Newspaper Antarc* Antarctic Università degli Studi di Napoli "Parthenope": CINECA IRIS Antarctic The Antarctic The Landing ENVELOPE(-45.689,-45.689,-60.733,-60.733) Advances in Space Research 66 8 1876 1886
spellingShingle DUSTER Flight Simulation Predictor
Numerical simulation
Zero–pressure balloons
Liuzzi V.
Della Corte V.
Rotundi A.
Ivanovski S.
Dionnet Z.
Brunetto R.
Inno L.
Zero-pressure balloons trajectory prediction: Duster flight simulations
title Zero-pressure balloons trajectory prediction: Duster flight simulations
title_full Zero-pressure balloons trajectory prediction: Duster flight simulations
title_fullStr Zero-pressure balloons trajectory prediction: Duster flight simulations
title_full_unstemmed Zero-pressure balloons trajectory prediction: Duster flight simulations
title_short Zero-pressure balloons trajectory prediction: Duster flight simulations
title_sort zero-pressure balloons trajectory prediction: duster flight simulations
topic DUSTER Flight Simulation Predictor
Numerical simulation
Zero–pressure balloons
topic_facet DUSTER Flight Simulation Predictor
Numerical simulation
Zero–pressure balloons
url http://hdl.handle.net/11367/86133
https://doi.org/10.1016/j.asr.2020.07.011