Csilla Orgel

ORCID: 0000-0001-7317-0092
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About
Contact & Profiles
Research Areas
  • Planetary Science and Exploration
  • Astro and Planetary Science
  • Space Exploration and Technology
  • Geology and Paleoclimatology Research
  • Space Science and Extraterrestrial Life
  • Spacecraft Design and Technology
  • Methane Hydrates and Related Phenomena
  • Spaceflight effects on biology
  • Maritime and Coastal Archaeology
  • Spacecraft and Cryogenic Technologies
  • Scientific Research and Discoveries
  • Aerospace Engineering and Energy Systems
  • Aeolian processes and effects
  • Amazonian Archaeology and Ethnohistory
  • Geological Studies and Exploration
  • Geological formations and processes
  • Hydrocarbon exploration and reservoir analysis
  • Opportunistic and Delay-Tolerant Networks
  • Marine and environmental studies
  • Satellite Communication Systems
  • Robotics and Sensor-Based Localization
  • Image Processing and 3D Reconstruction
  • Atmospheric and Environmental Gas Dynamics
  • Space exploration and regulation
  • Evolution and Paleontology Studies

Freie Universität Berlin
2016-2024

European Space Research and Technology Centre
2020-2024

European Space Agency
2022

Institut für Lungenforschung
2017-2018

Planet
2017-2018

Space Research Institute
2014

Eötvös Loránd University
2013-2014

Abstract The South Pole–Aitken (SPA) basin is the oldest and largest visible impact structure on Moon, making it a high priority science site for exploration missions. 492 km diameter Apollo peak-ring one of youngest basins within SPA basin. We selected three regions interest (ROIs) in which landing operational hazards are minimized evaluated their situ resource utilization (ISRU) potential. examined topography, slope, crater density, rock abundance, geologic mapping, mineralogy, inferred...

10.3847/psj/ad1108 article EN cc-by The Planetary Science Journal 2024-02-01

Abstract The lunar cratering record provides valuable information about the late accretion history of inner solar system. However, our understanding origin, rate, and timing impacting projectiles is far from complete. To learn more these projectiles, we can examine crater size‐frequency distributions (CSFDs) on Moon. Here reinvestigate populations 30 basins (≥ 300 km) using buffered nonsparseness correction technique, which takes obliteration into account, thus providing accurate...

10.1002/2017je005451 article EN Journal of Geophysical Research Planets 2018-02-07

Abstract We conducted a detailed photogeological analysis of the northern portion South Pole‐Aitken (SPA) basin (10–60°S, 125–175°W) and compiled geological map (1:500,000 scale) this region. Our new absolute model age for Apollo basin, 3.98 + 0.04/−0.06 Ga, provides lower limit formation SPA basin. Some plains units in study area were formed by distal ejecta from remote craters basins. The characteristic concentrations FeO TiO 2 other are indicative their volcanic origin. oldest materials...

10.1029/2018je005590 article EN cc-by-nc-nd Journal of Geophysical Research Planets 2018-09-17

We report on the MARS2013 mission, a 4-week Mars analog field test in northern Sahara. Nineteen experiments were conducted by crew Morocco under simulated martian surface exploration conditions, supervised Mission Support Center Innsbruck, Austria. A Remote Science team analyzed data near real time, providing planning input for management of complex system assets; two advanced space suit simulators, four robotic vehicles, an emergency shelter, and stationary sensor platform realistic work...

10.1089/ast.2013.1062 article EN Astrobiology 2014-05-01

Abstract We used a grid‐mapping technique to analyze the distribution of 13 water‐ and ice‐related landforms in Acidalia Planitia as part joint effort study three main basins northern lowlands Mars, that is, Acidalia, Utopia, Arcadia Planitiae. The were mapped at full Context Camera resolution along 300‐km‐wide strip from 20°N 84°N. identified four landform assemblages: (1) Geologically recent polar cap (massive ice), which superposes latitude‐dependent mantle (LDM) (LA1); (2) landforms,...

10.1029/2018je005664 article EN Journal of Geophysical Research Planets 2018-09-13

Abstract This work in Utopia Planitia is the first continuous regional mapping of ice‐related landforms integrated into an effort to study three main basins (Arcadia, Acidalia, and Planitiae) northern plains. The distribution morphotypes these landforms, SHAllow RADar detections, crater size‐frequency measurements (>50 m diameter) were used understand permafrost cryolithology its past evolution relation climate Planitia. Three assemblages identified based on their spatial correlation with...

10.1029/2018je005665 article EN Journal of Geophysical Research Planets 2018-09-13

This 1:30,000 scale geological map describes Oxia Planum, Mars, the landing site for ExoMars Rosalind Franklin rover mission. The represents our current understanding of bedrock units and their relationships prior to Franklin's exploration this location. details 15 organised into 6 groups 7 textural surficial units. were identified using visible near-infrared remote sensing datasets. objectives are (i) identify where most astrobiologically relevant rocks likely be found, (ii) show hypotheses...

10.1080/17445647.2024.2302361 article EN cc-by Journal of Maps 2024-03-22

After the successful landing of Mars Science Laboratory rover, both NASA and ESA initiated a selection process for potential sites Mars2020 ExoMars missions, respectively. Two ellipses located in Mawrth Vallis region were proposed evaluated during series meetings (three mission five ExoMars). We describe here regional context two as well framework objectives these missions. Key science targets their astrobiological interests are reported. This work confirms that contain multiple past martian...

10.1089/ast.2019.2074 article EN Astrobiology 2020-01-09

Abstract The crater record of a planetary surface unit is often analyzed by its cumulative size‐frequency distribution (CSFD). Measuring CSFDs involves traditional approaches, such as counting (TCC) and buffered (BCC), well geometric corrections, nonsparseness correction (NSC) (BNSC). NSC BNSC consider the effects obliteration on CSFD. On Moon, leads to two distinct states in which obtained do not match production CSFD—crater equilibrium nonsparseness. Crater occurs when each new impact...

10.1029/2019je006273 article EN cc-by Journal of Geophysical Research Planets 2020-04-01

We present the geography of Oxia Planum, landing site for ExoMars 2022 mission. This map provides planetary science community with a framework to understand this, until recently, unexplored area. The comprises (1) mosaic panchromatic Context Camera (CTX) Digital Elevation Models (DEM) and Ortho Rectified Images (ORI) controlled High Resolution Stereo (HRSC) multiorbit (2) Colour Surface Imaging System (CaSSIS) synthetic colour data products, registered CTX ORI mosaic. define grid exploration...

10.1080/17445647.2021.1982035 article EN cc-by Journal of Maps 2021-11-09

With the renewed interest in lunar surface exploration, European Space Agency envisions to stimulate creation of communications and navigation services (LCNS) enable, among others, autonomous capabilities for rovers. As number satellites foreseen such a service is much smaller compared Earth-based global satellite systems, different complementary technologies are pursued improve attainable accuracy One way position provided by LCNS constrain their vertical using high resolution digital...

10.3390/rs14163942 article EN cc-by Remote Sensing 2022-08-14

<p>The south polar region is an area of renewed interest lunar exploration because the presence volatiles including water ice at surface or just beneath (e.g., Deutsch <em>et al.,</em> 2020, Hayne al</em>.,2015, Kring al</em>., Lemelin 2021, Li 2018). PROSPECT instrument selected for flight on 10<sup>th</sup> NASA Commercial Lunar Payload Services (CLPS) mission and aims to sample up 1 m depth....

10.5194/epsc2022-530 preprint EN 2022-09-23

Abstract The analysis of crater size‐frequency distributions (CSFDs) is a widely used technique to date and investigate planetary surface processes. There are two well‐established measurement techniques, traditional counting buffered counting, new geometric corrections, nonsparseness correction correction. techniques consider the effects obliteration subsequent recratering while measuring CSFDs in areas high density. Currently, ArcGIS add‐in CraterTools can be apply techniques. tool relies...

10.1002/2018ea000383 article EN cc-by-nc-nd Earth and Space Science 2018-05-19

Abstract A project of mapping ice‐related landforms was undertaken to understand the role subsurface ice in northern plains. This work is first continuous regional from CTX ( ConTeXt Camera , 6 m/pixel; Malin et al., ) imagery Arcadia Planitia along a strip 300 km across stretching 30°N 80°N centered on 170°W line longitude. The distribution and morphotypes these were used permafrost cryolithology. mantled textured signatures occur almost ubiquitously between 35°N 78°N have positive spatial...

10.1029/2018je005663 article EN Journal of Geophysical Research Planets 2018-09-14

Abstract Mercury has one of the best‐preserved impact records in inner solar system due to absence an atmosphere and relatively unmodified ancient surface. However, our knowledge early record nature impacting projectiles are far from complete. To get a better understanding history, we examined large basins ( D ≥ 300 km) on Mercury. Here cataloged 94 basins, 80 which classify as certain or probable, 1.7 times more than previously recognized. We re‐evaluate crater densities using buffered...

10.1029/2019je006212 article EN cc-by Journal of Geophysical Research Planets 2020-04-30

Aeolian and fluvial processes on Earth show significant interactions. Within terrestrial desert environments, analysis of ~200 locations has revealed that where ephemeral or episodic rivers flow across a dune field the predominant alternate between aeolian fluvial, when dunes are active, they interact with one another. Avulsions can be major, channels in northern Kalahari having cumulative diversions 10s km. Considering Mars likely had an arid environment during period peak activity,...

10.5194/egusphere-egu23-2810 preprint EN 2023-02-22

In deserts on Earth, aeolian (wind-blown) and fluvial (river) (AF) processes display considerable interactions, which have an impact dune river trajectories, morphologies, geometries, distributions. These interactions can lead to water loss the subsurface formation of sabkhas, are interdune ponds that transform into salt flats. pools where primordial continental life Earth is hypothesized emerged, evidenced by microbial mats. Lithified dunes interwoven inverted channels, discovery aqueously...

10.5194/egusphere-egu24-18586 preprint EN 2024-03-11

MARS2013 was an integrated Mars analog field simulation in eastern Morocco performed by the Austrian Space Forum between February 1 and 28, 2013. The purpose of this paper is to discuss system data processing utilization adopted Remote Science Support (RSS) team during mission. RSS procedures were designed optimize operational efficiency Flightplan, crew, teams a long-term mission with introduced 10 min time delay communication "Mars" Earth. workflow centered on single-file, easy-to-use,...

10.1089/ast.2013.1071 article EN Astrobiology 2014-04-30

We have developed a portable dual-wavelength laser fluorescence spectrometer as part of multi-instrument optical probe to characterize mineral, organic, and microbial species in extreme environments. Operating at 405 532 nm, the instrument was originally designed for use by human explorers produce laser-induced emission (L.I.F.E.) spectral database mineral organic molecules found communities Earth's cryosphere. Recently, our team had opportunity explore strengths limitations when it deployed...

10.1089/ast.2013.1081 article EN Astrobiology 2014-05-01

Abstract Impact crater records on planetary surfaces are often analyzed for their spatial randomness. Generalized approaches such as the mean second closest neighbor distance (M2CND) and standard deviation of adjacent area (SDAA) available via a software tool but do not take influence curvature into account in current implementation. As result, measurements affected by map distortion effects can lead to wrong interpretations. This is particularly critical investigations global data sets...

10.1029/2020je006693 article EN Journal of Geophysical Research Planets 2021-02-10
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