An interactive vizualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars N Balint Zita, Székely Balázs, Kovács Gábor.

Slides:



Advertisements
Similar presentations
GEOLOGY OF PHOBOS-GRUNT LANDING SITES: A VIEW FROM THE MEX HRSC IMAGES. Vernadsky Institute, Moscow C. Lorenz, A. Basilevsky K. Willner Technical University,
Advertisements

Seismic Stratigraphy EPS 444
A COMPARISON OF HOMOGENEOUS AND MULTI-LAYERED BERM BREAKWATERS WITH RESPECT TO OVERTOPPING AND STABILITY Lykke Andersen, Skals & Burcharth ICCE2008, Hamburg,
ON WIDTH VARIATIONS IN RIVER MEANDERS Luca Solari 1 & Giovanni Seminara 2 1 Department of Civil Engineering, University of Firenze 2 Department of Environmental.
New modules of the software package “PHOTOMOD Radar” September 2010, Gaeta, Italy X th International Scientific and Technical Conference From Imagery to.
LING 111 Teaching Demo By Tenghui Zhu Introduction to Edge Detection Image Segmentation.
Streamlined Islands and Craters
Environmental and Exploration Geophysics I tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Workshop on Earth Observation for Urban Planning and Management, 20 th November 2006, HK 1 Zhilin Li & Kourosh Khoshelham Dept of Land Surveying & Geo-Informatics.
Small valleys in the southern part of the ellipse Long/lat: E, 23.85N Rational: Sediments deposited in this partly filled valley may be of utmost.
Oyama layered deposits Long/lat: from E, 24.00N to E, 23.20N Rational: Clays have been transported onto the floor of Oyama and deposited as.
Eroded Crater at Mawrth: at least 2 generations of fill. Latitude/longitude: 24° 2'20"N, 18°56'20"W (previously proposed but with different rationale)
The Mawrth Vallis Phyllosilicates Within a Regional Context: Extent, stratigraphy, and mineralogy of Phyllosilicates around Mawrth Vallis and Western Arabia.
Mars Mapping Mission St Joseph School Mr. Serra’s 7 TH Grade 4/19/2007 Presenter: Ms. Batchelder.
Experimental Methods  Solutions were prepared of 10, 15, 20, 25 wt% MgSO 4 ; and 10.9, 13.7, 17.8, and 18.0 wt% FeSO 4  Experimental conditions inside.
A WAIS Analog Found on Mars Polar Cap Weili Wang 1, Jun Li 1 and Jay Zwally 2 1. Raytheon ITSS, NASA/GSFC, Code 971, Greenbelt, MD 20771, USA. 2. Ocean.
Maryam Sadeghi 1,3, Majid Razmara 1, Martin Ester 1, Tim K. Lee 1,2,3 and M. Stella Atkins 1 1: School of Computing Science, Simon Fraser University 2:
GROOVES OF PHOBOS AS SEEN ON THE MEX HRSC RECTIFIED IMAGES AND COMPARISONS WITH PLANETERY ANALOGS A.T. Basilevsky 1, J. Oberst 2,3, K. Willner 3, M. Waehlisch.
Chapter 3 Section 1- Finding Locations on Earth
Texture. Texture is an innate property of all surfaces (clouds, trees, bricks, hair etc…). It refers to visual patterns of homogeneity and does not result.
Mars Project(s): tasks Using Mars Express HRSC & other datasets.
EDGE DETECTION USING MINMAX MEASURES SOUNDARARAJAN EZEKIEL Matthew Lang Department of Computer Science Indiana University of Pennsylvania Indiana, PA.
Student: Danielle Clarke and Mentor: Briony Horgan ASU/NASA Space Grant Program.
Discussion of High Thermal Inertia Craters on Mars in the Isidis and Syrtis Major Regions Jordana Friedman Arizona State University.
Photometric analysis of Martian moon Phobos with the HRSC on Mars Express A. Pasewaldt 1, K. Willner 2, J. Oberst 1,2, Frank Scholten 1, M. Wählisch 1,
Slide: 1 The first Moscow Solar System Symposium (1M-S3) >> Phobos Digital Terrain Model (DTM)and Coordinate Refinement for Phobos-Grunt Mission Support.
Sensitivity analysis of hydraulic model to morphological changes and changes in flood inundation extent J.S. Wong 1, J. Freer 1, P.D. Bates 1, & D.A. Sear.
Magnetic Anomaly Map Including outline of island Magnetic Anomalies of Macquarie Island.
Software used: ArcMap , MatLab R2015b, Google Earth 7.1.5
C.M. Rodrigue, 2014 Geography, CSULB Mars: Fourth Order Landscapes Geography 441/541 S/14 Dr. Christine M. Rodrigue.
PROPOSED MARS LANDING SITES FOR MER A & B West Hemisphere Centered at: 30°N, 30°W East Hemisphere Centered at: 30°N, 210°W 10°N 15°S 0° O OO O O 10°N 15°S.
Transient response of the ionosphere to X-ray solar flares Jaroslav Chum (1), Jaroslav Urbář (1), Jann-Yenq Liu (2) (1) Institute of Atmospheric Physics,
REGOLITH LANDFORM MAPPING OF MERIDIANI PLANUM AND SURROUNDS J. D. A. Clarke 1 C. F. Pain 2 and M. Thomas 1, 1 Australian Centre for Astrobiology, Macquarie.
References: [1] E. Tognoli, J. Lagarde, G.C. DeGuzman, J.A.S. Kelso (2006). The phi complex as a neuromarker of human social coordination. PNAS 104:
Estimating Quality of Canola Seed Using a Flatbed Scanner.
UBC/UW 2011 Hydrology and Water Resources Symposium Friday, September 30, 2011 DIAGNOSIS OF CHANGING COOL SEASON PRECIPITATION STATISTICS IN THE WESTERN.
Continuous wavelet transform of function f(t) at time relative to wavelet kernel at frequency scale f: "Multiscale reconstruction of shallow marine sediments.
Models of the Earth Section 3 Section 3: Types of Maps Preview Key Ideas Topographic Maps Topographic Maps and Contour Lines Index Contour, Contour Interval,
Color Image Segmentation Mentor : Dr. Rajeev Srivastava Students: Achit Kumar Ojha Aseem Kumar Akshay Tyagi.
Vision Based hand tracking for Interaction The 7th International Conference on Applications and Principles of Information Science (APIS2008) Dept. of Visual.
Shadow Detection in Remotely Sensed Images Based on Self-Adaptive Feature Selection Jiahang Liu, Tao Fang, and Deren Li IEEE TRANSACTIONS ON GEOSCIENCE.
Impact craters are geologic structures formed when a large meteoroid, asteroid or comet smashes into a planet or a satellite.Impact craters are geologic.
EPISODICITY OF VOLCANIC AND FLUVIAL PROCESSES ON MARS G. Neukum1, A.T. Basilevsky1,2, and the HRSC Team 1Freie Universitaet Berlin, Malteserstr., ,
Introduction: The Mawrth Vallis region has been identified by the Mars Express OMEGA and MRO CRISM instruments as a region with abundant hydrated phyllosilicate.
C.M. Rodrigue, 2007 Geography, CSULB Boldly Going Where No Geographer Has Gone Before: The Martian Classroom The Los Angeles Geographical Society (7 September.
Wet environment reconstruction using IR spectra on Mars Akos Kereszturi Konkoly Astronomical Institute, MTA CSFK Mars Astrobiology Group (ESA RCL) OTKA.
Models of the Earth Section 3 Section 3: Types of Maps Preview Key Ideas Topographic Maps Topographic Maps and Contour Lines Index Contour, Contour Interval,
Parts of a Map. o Title o Data frame o Labels o Compass (compass rose) o Legend (Key) o Scale o Colors.
Anthony Alvarado, PE, CFM National Hydraulic Engineering Conference
Automated airway evaluation system for multi-slice computed tomography using airway lumen diameter, airway wall thickness and broncho-arterial ratio B.
Małgorzata Jenerowicz Space Research Centre,
(Lots of pretty pictures. No math.)
LANDFORMS Chapter 6- Lesson 1.
Terrain Represent the “Surface” of the Earth
Chapter 3 Section 3 Types of Maps Objectives
Fresh Exposures of Hydrous Fe-bearing Amorphous Silicates on Mars
Clark R. Chapman Southwest Research Inst. Boulder, CO USA
EROSION.
Craters on Mars DRAFT Google Earth.
Intelligent Interpretation: From Here to Where?
DTM colourisation tool
Chapter 1, Lesson 2, Topographic and Geologic Maps 1
Toshiro Oda, Keiichi Namba, Yuichiro Maéda  Biophysical Journal 
Chapter 1, Lesson 2, Topographic and Geologic Maps 1
R.A. Yingst, F.C. Chuang, D.C. Berman, S.C. Mest
EROSION.
by M. P. Golombek, R. A. Cook, T. Economou, W. M. Folkner, A. F. C
Stratigraphic Analysis of the Distributary Fan in Holden NE Crater
by Hansjoerg J. Seybold, Edwin Kite, and James W. Kirchner
Classification of Morphology of Interacting Galaxy Systems
Presentation transcript:

An interactive vizualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars N Balint Zita, Székely Balázs, Kovács Gábor Department of Geophysics and Space Sciente, ELTE

Introduction HRSC (High Resolution Stereo Camera) Nanedi Valles Local slope histograms Data visualization and processing : own program code RGB (red, green, blue) Current and future goals Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 2

Data Vienna University of Technology, IPF Within the framework of TMIS.ascrea project calculate the local slope histograms with own programe code Mars Express HRSC high-resolution stereo color camera 9 CCD-line 3 stereo-channels (Nadir, Stereo I and Stereo 2) Recording>> DTM>> slope histograms ESA Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 3

NANEDI VALLES southwest-northeast orientation region of Xanthe Terra extends roughly 800 km, the valley ranges from  approximately 0.8 to 5 km wide, 0.5 km depth relatively flat-floored, steep-sloped, exhibits meanders merging of two branches in the north 40 km Goggle Mars Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 4

The significance of the research area Morphologically rich area The origin of the valley is not yet clear, but it seems likely that it is from fluvial erosion Bandeira et al., 2012, Adv. Space Res. Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 5

Presentation of histograms NI LabView 2011 Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 6

River bed Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 7

Valley sides Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 8

Schematic cross section for a typical central peak crater NASA Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 9

Impact crater Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 10

Impact crater Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 11

Impact crater Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 12

Significance of slope histograms Geological aspects : Erosion Rock quality Development Detection of morphological units Google Mars Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 13

Skewness Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 14

RGB (red, green, blue) 15 Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars

Red – Mode amplitude Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 16

Green - Skewness Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 17

Blue - Standard deviation Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 18

RGB Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 19

RGB Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 20

Thank you for your attention! Conclusions, further plans Study based on skewness Classification based on Kolmogorov distance criteria Thank you for your attention! Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars 21

Előzmények Source: A Method for Automated Extraction of Martian Talus Slopes – Case Studies of Nanedi Valles and West Candor Chasma, Mars B. Székely, T. Podobnikar 22 Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars

Lejtőszög-hisztogram osztályozás felhasználása Keleti-Alpok lejtőszög-hisztogram térkép Keleti-Alpok lepusztulás-történeti térkép Source: Neotectonic movements and their geomorphic response as reflected in surface parameters and stress patterns in the Eastern Alps B. Szekely ´*, J. Reinecker†, I. Dunkl††, W. Frisch , and J. Kuhlemann 23 Balint Zita: An interactive visualisation and evaluation tool for DTM-derived slope histograms of Nanedi Valles region, Mars