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  • 1
    Keywords: Forschungsbericht ; Satellitenfernerkundung ; Radar ; Synthetische Apertur ; Interferometrie ; Dauerfrostboden ; Senkung
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (77 Seiten, 39,68 MB) , Illustrationen, Diagramme
    Language: German
    Note: Förderkennzeichen BMWi 50EE1418 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
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  • 2
    Publication Date: 2023-02-24
    Description: We have generated a digital elevation model (DEM) of an area between the town of Inuvik and Eskimo Lakes near the Mackenzie Delta, Northwest Territories, Canada. We used seven TanDEM-X CoSSC pairs, acquired in summer 2015 during the TanDEM-X Science Phase, and provide here the mean elevation of the seven produced DEMs (GeoTIFF raster). The processing was based on differential SAR interferometry with the use of ArcticDEM as reference. We also provide the standard deviation map of the seven DEMs (GeoTIFF raster) as a quality indicator. The final mean DEM was validated against DGPS measurements. Height values are given in meters in reference to ellipsoid (WGS84). The pixel size of the products is 10 m. The coordinate reference system is UTM Zone 8N WGS84. Detailed description of the TanDEM-X data, interferometric processing, and the validation is given in the attached metadata file.
    Keywords: AWI Arctic Land Expedition; CA-Land_2016_TrailValleyCreek; CoSSC; DEM; Northwest Territories, Canada; PermaSAR; PermaSAR: Development of a Method to Detect Subsidence by Means of D-InSAR in Permafrost Regions; SAT; Satellite remote sensing; TanDEM-X; Trail_Valley_Creek_area
    Type: Dataset
    Format: application/zip, 378.6 MBytes
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  • 3
    Publication Date: 2023-07-24
    Description: The datasets were acquired at the Arctic tundra site of Trail Valley Creek (TVC), Northwest Territories, Canada, which is underlain by continuous permafrost. With the objective to quantify thaw/freeze dynamics of the ground over time, the two study sites (about 50x50 m each) were repeatedly captured in June 2015, August 2015, and August 2016 by terrestrial laser scanning (TLS) and by Real-Time Kinematic (RTK) Global Navigation Satellite System (GNSS) measurements. Additionally, 24 fiberglass poles were anchored deep in the permafrost and, therefore, assumed to be motionless. With these poles, surface displacement was estimated by measuring repeatedly the distance between ground surface and the top of the poles in June 2015, August 2015, July 2016, August 2016 and June 2017. Furthermore, thaw depths were measured around each fiberglass pole. Additionally, one-time GNSS measurements of the ground surface elevation were acquired at a number of points outside of the two study sites.
    Keywords: AWI Arctic Land Expedition; CA-Land_2016_TrailValleyCreek; File content; File format; File name; File size; MULT; Multiple investigations; Northwest Territories, Canada; PermaSAR; PermaSAR: Development of a Method to Detect Subsidence by Means of D-InSAR in Permafrost Regions; Trail_Valley_Creek_2016-1; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
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  • 4
    Publication Date: 2018-01-19
    Description: Three-dimensional data acquired by terrestrial laser scanning (TLS) provides an accurate representation of the Earth’s surface, which is commonly used to detect and quantify topographic changes on a small scale. However, in Arctic permafrost regions TLS-based monitoring of thaw subsidence is challenging due to vegetation and the micro-topographic characteristics (e.g. dense moss-lichen layer, hummocks etc.). In this presentation, we focus, firstly, on the evaluation of raster- and point-based TLS methods for quantifying small-scale thaw subsidence within the continuous permafrost zone. Secondly, a new filter strategy is presented that reduces spatial sampling effects caused by various factors such as vegetation, micro-topography and scan-setup. Our study site is located at the Trail Valley Creek research watershed, 50 km north-east of Inuvik, Northwest Territories, Canada. Three field campaigns took place in 2015 and 2016. Besides capturing TLS data, at-point real-time kinematic (RTK) Global Navigation Satellite System (GNSS) measurements and manual subsidence measurements were gathered. To achieve a highly accurate registration (on mm-scale) of the three TLS campaigns, co-registration of the georeferenced point clouds is performed based on the stable fix points in the otherwise highly dynamic permafrost environment. Then, different methods to quantify vertical ground movements are applied and evaluated. The result reveals limitations of standard raster-based DEM differencing, but also of point-based distance calculation for detecting spatial patterns of small-scale thaw subsidence. In the Arctic tundra ecosystem, TLS-based deformation analysis is strongly affected by occlusion and spatial sampling effects, even if data acquisition is repeated from similar scan positions. We show that the mentioned errors can be reduced by capturing the ground surface from more than one TLS scan position. Our filter strategy allows to identify TLS points which are suitable for multi-temporal deformation analyses, and results in an average seasonal subsidence rate (2015/06-2015/08) of about -2.0 cm at our study site. The derived subsidence maps deliver highly accurate ground-truth data, which is needed to improve area-wide subsidence monitoring methods such as SAR interferometry. This leads to a deeper understanding of permafrost-related subsidence processes.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 5
    Publication Date: 2019-10-22
    Description: Etwa ein Viertel der nördlichen Hemisphäre ist von dauerhaft gefrorenem Boden, dem Permafrost, geprägt. Im Sommer taut die oberste Schicht des Permafrostes auf und gefriert im Winter wieder. Durch die starke Erwärmung des arktischen Klimas taut der Boden im Sommer tiefer auf als bisher. In südlichen Gebieten der Arktis kommt Permafrost nur noch vereinzelt vor (diskontinuierlich oder sporadisch). Durch die Erwärmung kann Permafrost in diesen Gebieten sogar komplett verschwinden. Wenn Permafrost im Sommer auftaut, schmilzt das im Boden gespeicherte Eis. Dadurch verringert sich das Bodenvolumen und die Landoberfläche senkt sich in vielen Gebieten der Arktis. Zwar findet während der Gefrierperiode oftmals wieder eine Hebung statt. Jedoch konnte in den vergangenen Jahren in einigen Gebieten eine Nettosenkung - auch Subsidenz genannt - beobachtet werden. Diese ist auf die ansteigenden Temperaturen und die damit verbundenen höheren Auftauraten zurückzuführen. Das verstärkte Tauen des Permafrostbodens hat schwerwiegende Folgen für Ökosysteme, Infrastruktur und die ansässige Bevölkerung mit sich. Es ist daher sowohl für die Wissenschaft, als auch für Wirtschaft und Politik essentiell, diese Vorgänge quantifizieren zu können.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Miscellaneous , notRev
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  • 6
    Publication Date: 2020-02-17
    Description: Surface dynamics, such as subsidence and heave, as a result of permafrost thawing and freezing is a well-known phenomenon. Ground measurements are indicating that such movements exist and first attempts to use satellite data to detect these changes on a larger scale have been undertaken. In particular data from radar satellites have been used to generate differential interferograms (D-InSAR) in order to detect areas of movements. However there are still many uncertainties and limitations related to this method, such as the influence of vegetation and microtopography on the radar signal. Within the PermaSAR project a multi-source approach, using TanDEM-X data, ground truth measurements (subsidence stations and RTK GNSS), but also highly precise terrestrial 3D LiDAR data shall help to identify influences of the captured surface characteristics on high-resolution D-InSAR. In a subsequent working step the identified influences will be quantified and a method developed in order to mask, reduce, or even eliminate, these effects. For the study, a region in Northwest Canada, 50 km North of Inuvik has been chosen. The site, so-called Trail Valley Creek, lies in the continuous permafrost zone and the thickness of the permafrost is up to 370 m. The dominant vegetation in the basin are open tundra areas consist mostly of grasses, lichens and mosses. Research activities of the past reveal a potential of subsidence due to permafrost thawing in this region. In 2015 two field campaigns in the region could be realized: One in early June, after the freezing period and one in late August at the end of the thawing period. During the first campaign 8 automated ground temperature loggers and manual 24 subsidence stations were installed. Active layer thaw depth, as well as subsidence was recorded at 12 sites manually. During both campaigns the high-performance terrestrial LiDAR system Riegl VZ-400 was used to survey at two different sites (40 × 50 m) the microtopography and vegetation in 3D. The used LiDAR has full-waveform recording, with each single 3D measurement having a range precision and accuracy of about 3-5 mm at 100 m. Both test sites have been scanned with a point spacing of 3 mm at a distance of 10 m from 7 different scan positions. Additionally the Leica GNSS RTK GS10/GS15 system was used to get exact information about ground height and coordinates of certain features. First results indicate i) a very good co-registration of the LiDAR data and RTK GNSS data of the two campaigns and ii) a high correlation between the subsidence records of the LiDAR data, the RTK GNSS records and the subsidence stations. The corresponding mean subsidence rates derived from the three independent sources (LiDAR, GNSS RTK and subsidence stations) range from -2.31 cm (LiDAR) to -2.72 cm (subsidence station) (std. deviations from 0.89 (LiDAR) to 1.01 (subsidence station)). First analysis of subsidence using the TanDEM-X data are shown and compared to our multi-source ground truth measurements.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 7
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    In:  EPIC3Journal of Geological Resource and Engineering, 4, pp. 217-221
    Publication Date: 2015-03-28
    Description: The Polar Regions play an important role in the global processes of our planet, from climate change to sea level rise, protection from UV (ultraviolet) radiation to uptake of carbon dioxide. In addition, their scientific importance, extraordinary beauty and adventurous history provide perfect ingredients for both education and public outreach.Polar examples provide an excellent way to transmit basic concepts about a wide range of STEM (science, technology, engineering and mathematics) disciplines. The IPY (International Polar Year) brought educators and scientists together and provided the incentive for the formation of the PEI (Polar Educators International), an organization encouraging the exchange of ideas between educators and researchers and enhancement of the profile of polar education on the international scene. Educators must be adequately informed about current scientific polar research and have the confidenceto teach it to students. Scientists have the knowledge and data to explain these complexities, but may lack the communication skills to make the subject accessible to non-technical audiences. The development of this new network between polar educators and scientists has the potential to break down walls that restrict international collaboration and understanding, provide educators with topical and reliable information and share best practices internationally in an effective way.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
    Format: application/pdf
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  • 8
    Publication Date: 2015-04-01
    Description: Recent land cover changes in the Umiujaq region of northern Québec, Canada, have been quantified in order to estimate changes in the extent of discontinuous permafrost that strongly affect the forest-tundra ecotone. Changes in the areas covered by different vegetation types, thermokarst lakes, and degradation of lithalsas, have been investigated over an area of 60 km², extending from widespread discontinuous permafrost in the north to areas of scattered permafrost in the south, and from Hudson Bay in the west to the Lac Guillaume-Delisle graben 10 km further east. We used high resolution remote-sensing images (QuickBird 2004, GeoEye 2009) and four Landsat scenes (1986, 1990, 2001, 2008) as well as ground based data (vegetation, active layer thickness (ALT), snow parameters) collected between 2009 and 2011. Two change detection methods applied to estimate the land cover changes between 1986 and 2009 showed an overall increase in vegetation extent between 1986 and 2009, and a 21% increase in tall vegetation (spruce and tall shrubs) between 2004 and 2009 at the expense of low vegetation (lichens, prostrate shrubs, herbaceous vegetation). Thermokarst lakes and lithalsas in 10 sub-areas were mapped manually from satellite imagery. The area covered by water decreased by 24% between 2004 and 2009, often due to vegetation colonizing the margins of lakes, and ninety three of the observed lakes disappeared completely over that period. The area covered by lithalsas declined by 6%. Our results demonstrate the viability of using high resolution satellite imagery to detect changes in the land surface that can serve as indicators of permafrost degradation in the sub-Arctic.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
    Format: application/pdf
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  • 9
    Publication Date: 2015-09-27
    Description: Journal of Proteome Research DOI: 10.1021/acs.jproteome.5b00131
    Print ISSN: 1535-3893
    Electronic ISSN: 1535-3907
    Topics: Chemistry and Pharmacology
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