Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-901-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/se-5-901-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
01 Sep 2014
Research article |
| 01 Sep 2014
Sedimentological characteristics of ice-wedge polygon terrain in Adventdalen (Svalbard) – environmental and climatic implications for the late Holocene
Institute of Geography and Spatial Planning – Centre for Geographical Studies, University of Lisbon, Lisbon, Portugal
G. Vieira
Institute of Geography and Spatial Planning – Centre for Geographical Studies, University of Lisbon, Lisbon, Portugal
CERENA/University of Lisbon, Lisbon, Portugal
P. Pereira
Environmental Management Center, Mykolas Romeris University, Ateities St. Vilnius, Lithuania
M. Neves
Environmental Management Center, Mykolas Romeris University, Ateities St. Vilnius, Lithuania
M. C. Freitas
Universidade de Lisboa, Faculdade de Ciências, Centro de Geologia, Lisbon, Portugal
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Josep Bonsoms, Juan I. López-Moreno, Esteban Alonso-González, César Deschamps-Berger, and Marc Oliva
Nat. Hazards Earth Syst. Sci., 24, 245–264, https://doi.org/10.5194/nhess-24-245-2024, https://doi.org/10.5194/nhess-24-245-2024, 2024
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Climate warming is changing mountain snowpack patterns, leading in some cases to rain-on-snow (ROS) events. Here we analyzed near-present ROS and its sensitivity to climate warming across the Pyrenees. ROS increases during the coldest months of the year but decreases in the warmest months and areas under severe warming due to snow cover depletion. Faster snow ablation is anticipated in the coldest and northern slopes of the range. Relevant implications in mountain ecosystem are anticipated.
M. Fritz, B. N. Deshpande, F. Bouchard, E. Högström, J. Malenfant-Lepage, A. Morgenstern, A. Nieuwendam, M. Oliva, M. Paquette, A. C. A. Rudy, M. B. Siewert, Y. Sjöberg, and S. Weege
The Cryosphere, 9, 1715–1720, https://doi.org/10.5194/tc-9-1715-2015, https://doi.org/10.5194/tc-9-1715-2015, 2015
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This is a contribution about the future of permafrost research to the 3rd International Conference on Arctic Research Planning 2015 (ICARP III).
We summarize the top five research questions for the next decade of permafrost science from the perspective of early career researchers (ECRs).
We highlight the pathways and structural preconditions to address these research priorities.
This manuscript is an outcome of a community consultation conducted for and by ECRs on a global level.
A. Gómez-Ortiz, M. Oliva, F. Salvador-Franch, M. Salvà-Catarineu, D. Palacios, J. J. de Sanjosé-Blasco, L. M. Tanarro-García, J. Galindo-Zaldívar, and C. Sanz de Galdeano
Solid Earth, 5, 979–993, https://doi.org/10.5194/se-5-979-2014, https://doi.org/10.5194/se-5-979-2014, 2014
Eduardo Soares Nascimento, Allan Alves Lopes Ferreira, Guilherme Pina Cardim, Pedro Pina, and Erivaldo Antonio da Silva
ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., X-3-2024, 245–251, https://doi.org/10.5194/isprs-annals-X-3-2024-245-2024, https://doi.org/10.5194/isprs-annals-X-3-2024-245-2024, 2024
Mohammad Farzamian, Teddi Herring, Gonçalo Vieira, Miguel Angel de Pablo, Borhan Yaghoobi Tabar, and Christian Hauck
The Cryosphere, 18, 4197–4213, https://doi.org/10.5194/tc-18-4197-2024, https://doi.org/10.5194/tc-18-4197-2024, 2024
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An automated electrical resistivity tomography (A-ERT) system was developed and deployed in Antarctica to monitor permafrost and active-layer dynamics. The A-ERT, coupled with an efficient processing workflow, demonstrated its capability to monitor real-time thaw depth progression, detect seasonal and surficial freezing–thawing events, and assess permafrost stability. Our study showcased the potential of A-ERT to contribute to global permafrost monitoring networks.
Josep Bonsoms, Juan I. López-Moreno, Esteban Alonso-González, César Deschamps-Berger, and Marc Oliva
Nat. Hazards Earth Syst. Sci., 24, 245–264, https://doi.org/10.5194/nhess-24-245-2024, https://doi.org/10.5194/nhess-24-245-2024, 2024
Short summary
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Climate warming is changing mountain snowpack patterns, leading in some cases to rain-on-snow (ROS) events. Here we analyzed near-present ROS and its sensitivity to climate warming across the Pyrenees. ROS increases during the coldest months of the year but decreases in the warmest months and areas under severe warming due to snow cover depletion. Faster snow ablation is anticipated in the coldest and northern slopes of the range. Relevant implications in mountain ecosystem are anticipated.
E. S. Nascimento, A. A. L. Ferreira, T. G. Godoy, C. F. M. Fontoura Júnior, G. P. Cardim, P. M. B. D. Pina, and E. A. da Silva
ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci., X-1-W1-2023, 851–856, https://doi.org/10.5194/isprs-annals-X-1-W1-2023-851-2023, https://doi.org/10.5194/isprs-annals-X-1-W1-2023-851-2023, 2023
C. Soncco, G. Vieira, G. Goyanes, and E. Castro
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLIII-B4-2022, 553–558, https://doi.org/10.5194/isprs-archives-XLIII-B4-2022-553-2022, https://doi.org/10.5194/isprs-archives-XLIII-B4-2022-553-2022, 2022
Gonçalo Vieira, Carla Mora, Pedro Pina, Ricardo Ramalho, and Rui Fernandes
Earth Syst. Sci. Data, 13, 3179–3201, https://doi.org/10.5194/essd-13-3179-2021, https://doi.org/10.5194/essd-13-3179-2021, 2021
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Fogo in Cabo Verde is one of the most active ocean island volcanoes on Earth, posing important hazards to local populations and at a regional level. The last eruption occurred from November 2014 to February 2015. A survey of the Chã das Caldeiras area was conducted using a fixed-wing unmanned aerial vehicle. A point cloud, digital surface model and orthomosaic with 10 and 25 cm resolutions are provided, together with the full aerial survey projects and datasets.
Mohammad Farzamian, Gonçalo Vieira, Fernando A. Monteiro Santos, Borhan Yaghoobi Tabar, Christian Hauck, Maria Catarina Paz, Ivo Bernardo, Miguel Ramos, and Miguel Angel de Pablo
The Cryosphere, 14, 1105–1120, https://doi.org/10.5194/tc-14-1105-2020, https://doi.org/10.5194/tc-14-1105-2020, 2020
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A 2-D automated electrical resistivity tomography (A-ERT) system was installed for the first time in Antarctica at Deception Island to (i) monitor subsurface freezing and thawing processes on a daily and seasonal basis and map the spatial and temporal variability of thaw depth and to (ii) study the impact of short-lived extreme meteorological events on active layer dynamics.
Jaroslav Obu, Sebastian Westermann, Gonçalo Vieira, Andrey Abramov, Megan Ruby Balks, Annett Bartsch, Filip Hrbáček, Andreas Kääb, and Miguel Ramos
The Cryosphere, 14, 497–519, https://doi.org/10.5194/tc-14-497-2020, https://doi.org/10.5194/tc-14-497-2020, 2020
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Little is known about permafrost in the Antarctic outside of the few research stations. We used a simple equilibrium permafrost model to estimate permafrost temperatures in the whole Antarctic. The lowest permafrost temperature on Earth is −36 °C in the Queen Elizabeth Range in the Transantarctic Mountains. Temperatures are commonly between −23 and −18 °C in mountainous areas rising above the Antarctic Ice Sheet, between −14 and −8 °C in coastal areas, and up to 0 °C on the Antarctic Peninsula.
Gonçalo Vieira, Carla Mora, and Ali Faleh
The Cryosphere, 11, 1691–1705, https://doi.org/10.5194/tc-11-1691-2017, https://doi.org/10.5194/tc-11-1691-2017, 2017
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The Toubkal is the highest massif in North Africa (4167 m). Landforms and deposits above 3000 m show the effects of frost action in the present-day geomorphological dynamics, but data on ground temperatures were lacking. In this study ground surface temperature data measured across an altitudinal transect are presented and analysed for the first time. The highlight is the possible occurrence of permafrost at an elevation of 3800 m, which may be of high ecological and hydrological significance.
Carla Mora, Juan Javier Jiménez, Pedro Pina, João Catalão, and Gonçalo Vieira
The Cryosphere, 11, 139–155, https://doi.org/10.5194/tc-11-139-2017, https://doi.org/10.5194/tc-11-139-2017, 2017
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We evaluate the use of high-resolution microwave satellite images from TerraSAR-X for mapping snow-patch distribution in ice-free areas of the maritime Antarctic (King George Island). The imagery was acquired simultaneously to ground truthing of snow. Image classification resulted in very high accuracy when discriminating between snow, water and bare ground. The method provides a solution for characterizing the snowmelt patterns in the ice-free areas of the Antarctic Peninsula.
Sandra Heleno, Magda Matias, Pedro Pina, and António Jorge Sousa
Nat. Hazards Earth Syst. Sci., 16, 1035–1048, https://doi.org/10.5194/nhess-16-1035-2016, https://doi.org/10.5194/nhess-16-1035-2016, 2016
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A method for semi-automatic landslide detection and mapping is presented and tested using a very high-resolution satellite image, sensed 3 days after a major damaging landslide event that occurred in Madeira Island (20 February 2010). The testing is developed in a 15 km2 wide area, where 95 % of the number of landslides scars is detected by this approach.
P. Pereira, A. Gimeìnez-Morera, A. Novara, S. Keesstra, A. Jordán, R. E. Masto, E. Brevik, C. Azorin-Molina, and A. Cerdà
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hessd-12-12947-2015, https://doi.org/10.5194/hessd-12-12947-2015, 2015
Revised manuscript has not been submitted
Short summary
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Road and railway embankments contribute importantly to soil and water losses in South-Eastern Spain. Comparing with other land uses as scrubland and citrus plantations, road and railway embankments increased exponentially the amount of sediment transport and runoff. Restoration programs are needed to decrease soil and water losses in these man-made infrastructures.
M. Fritz, B. N. Deshpande, F. Bouchard, E. Högström, J. Malenfant-Lepage, A. Morgenstern, A. Nieuwendam, M. Oliva, M. Paquette, A. C. A. Rudy, M. B. Siewert, Y. Sjöberg, and S. Weege
The Cryosphere, 9, 1715–1720, https://doi.org/10.5194/tc-9-1715-2015, https://doi.org/10.5194/tc-9-1715-2015, 2015
Short summary
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This is a contribution about the future of permafrost research to the 3rd International Conference on Arctic Research Planning 2015 (ICARP III).
We summarize the top five research questions for the next decade of permafrost science from the perspective of early career researchers (ECRs).
We highlight the pathways and structural preconditions to address these research priorities.
This manuscript is an outcome of a community consultation conducted for and by ECRs on a global level.
A. Gómez-Ortiz, M. Oliva, F. Salvador-Franch, M. Salvà-Catarineu, D. Palacios, J. J. de Sanjosé-Blasco, L. M. Tanarro-García, J. Galindo-Zaldívar, and C. Sanz de Galdeano
Solid Earth, 5, 979–993, https://doi.org/10.5194/se-5-979-2014, https://doi.org/10.5194/se-5-979-2014, 2014
P. Pereira, X. Úbeda, J. Mataix-Solera, M. Oliva, and A. Novara
Solid Earth, 5, 209–225, https://doi.org/10.5194/se-5-209-2014, https://doi.org/10.5194/se-5-209-2014, 2014
A. Novara, L. Gristina, J. Rühl, S. Pasta, G. D'Angelo, T. La Mantia, and P. Pereira
Solid Earth, 4, 381–385, https://doi.org/10.5194/se-4-381-2013, https://doi.org/10.5194/se-4-381-2013, 2013
P. Pereira, A. Cerdà, X. Úbeda, J. Mataix-Solera, D. Martin, A. Jordán, and M. Burguet
Solid Earth, 4, 153–165, https://doi.org/10.5194/se-4-153-2013, https://doi.org/10.5194/se-4-153-2013, 2013
C. Lira, M. Lousada, A. P. Falcão, A. B. Gonçalves, S. Heleno, M. Matias, M. J. Pereira, P. Pina, A. J. Sousa, R. Oliveira, and A. B. Almeida
Nat. Hazards Earth Syst. Sci., 13, 709–719, https://doi.org/10.5194/nhess-13-709-2013, https://doi.org/10.5194/nhess-13-709-2013, 2013
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The Münsterdorf sinkhole cluster: void origin and mechanical failure
Effect of structural setting of source volume on rock avalanche mobility and deposit morphology
Deep oceanic submarine fieldwork with undergraduate students: an immersive experience with the Minerve software
Determining the Plio-Quaternary uplift of the southern French Massif Central; a new insight for intraplate orogen dynamics
Spatio-temporal dynamics of sediment transfer systems in landslide-prone Alpine catchments
Sinkholes and uvalas in evaporite karst: spatio-temporal development with links to base-level fall on the eastern shore of the Dead Sea
Distinct element geomechanical modelling of the formation of sinkhole clusters within large-scale karstic depressions
A semi-automated algorithm to quantify scarp morphology (SPARTA): application to normal faults in southern Malawi
Combined effects of grain size, flow volume and channel width on geophysical flow mobility: three-dimensional discrete element modeling of dry and dense flows of angular rock fragments
Stepwise drying of Lake Turkana at the end of the African Humid Period: a forced regression modulated by solar activity variations?
A geological model for the management of subsurface data in the urban environment of Barcelona and surrounding area
The impact of standard preparation practice on the runoff and soil erosion rates under laboratory conditions
sUAS and their application in observing geomorphological processes
Assessment of combating-desertification strategies using the linear assignment method
Delineating small karst watersheds based on digital elevation model and eco-hydrogeological principles
Rainfall and human activity impacts on soil losses and rill erosion in vineyards (Ruwer Valley, Germany)
Relative tectonic activity classification in the Kermanshah area, western Iran
Degradation of buried ice and permafrost in the Veleta cirque (Sierra Nevada, Spain) from 2006 to 2013 as a response to recent climate trends
Maskevarri Ráhppát in Finnmark, northern Norway – is it an earthquake-induced landform complex?
Erosion rates deduced from seasonal mass balance along the upper Urumqi River in Tianshan
The role of karst in engineering and environmental geosciences
Optical method for measuring bed topography and flow depth in an experimental flume
Georg Kaufmann, Douchko Romanov, Ulrike Werban, and Thomas Vienken
Solid Earth, 14, 333–351, https://doi.org/10.5194/se-14-333-2023, https://doi.org/10.5194/se-14-333-2023, 2023
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We discuss collapse sinkholes occuring since 2004 on the sports field of Münsterdorf, a village north of Hamburg. The sinkholes, 2–5 m in size and about 3–5 m deep, develop in peri-glacial sand, with a likely origin in the Cretaceous chalk, present at about 20 m depth. The area has been analyzed with geophysical and direct-push-based methods, from which material properties of the subsurface have been derived. The properties have been used for mechanical models, predicting the subsidence.
Zhao Duan, Yan-Bin Wu, Qing Zhang, Zhen-Yan Li, Lin Yuan, Kai Wang, and Yang Liu
Solid Earth, 13, 1631–1647, https://doi.org/10.5194/se-13-1631-2022, https://doi.org/10.5194/se-13-1631-2022, 2022
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We studied the mobility and sedimentary characteristics of rock avalanches influenced by initial discontinuity sets with experimental methods. In the experiments, we set different initial configurations of blocks. The results revealed that the mobility and surface structures of the mass flows differed significantly. In the mass deposits, the block orientations were affected by their initial configurations and the motion processes of the mass flows.
Marianne Métois, Jean-Emmanuel Martelat, Jérémy Billant, Muriel Andreani, Javier Escartín, Frédérique Leclerc, and the ICAP team
Solid Earth, 12, 2789–2802, https://doi.org/10.5194/se-12-2789-2021, https://doi.org/10.5194/se-12-2789-2021, 2021
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We use the Minerve virtual reality software to bring undergraduate students to an unusual field trip at 1200 m below sea level in the Lesser Antilles area. This region is located above an active subduction zone responsible for intense volcanic and seismic activity. In particular, we focus on the Roseau submarine fault that ruptured during the Mw 6.3 Les Saintes earthquake and presented a fresh scarp that the students can analyze and map in VR. They compile their results in a GIS project.
Oswald Malcles, Philippe Vernant, Jean Chéry, Pierre Camps, Gaël Cazes, Jean-François Ritz, and David Fink
Solid Earth, 11, 241–258, https://doi.org/10.5194/se-11-241-2020, https://doi.org/10.5194/se-11-241-2020, 2020
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We aim to better understand the challenging areas that are the intraplate regions using one example: the southern French Massif Central and its numerous hundreds of meters deep valleys. We apply a multidisciplinary approach there using geomorphology, geochronology, and numerical modeling.
Our dating results show that the canyon incisions are part of the Plio-Quaternary evolution with incision rate of ~ 80 m Ma−1. We propose then that this incision is possible due to an active regional uplift.
François Clapuyt, Veerle Vanacker, Marcus Christl, Kristof Van Oost, and Fritz Schlunegger
Solid Earth, 10, 1489–1503, https://doi.org/10.5194/se-10-1489-2019, https://doi.org/10.5194/se-10-1489-2019, 2019
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Using state-of-the-art geomorphic techniques, we quantified a 2-order of magnitude discrepancy between annual, decadal, and millennial sediment fluxes of a landslide-affected mountainous river catchment in the Swiss Alps. Our results illustrate that the impact of a single sediment pulse is strongly attenuated at larger spatial and temporal scales by sediment transport. The accumulation of multiple sediment pulses has rather a measurable impact on the regional pattern of sediment fluxes.
Robert A. Watson, Eoghan P. Holohan, Djamil Al-Halbouni, Leila Saberi, Ali Sawarieh, Damien Closson, Hussam Alrshdan, Najib Abou Karaki, Christian Siebert, Thomas R. Walter, and Torsten Dahm
Solid Earth, 10, 1451–1468, https://doi.org/10.5194/se-10-1451-2019, https://doi.org/10.5194/se-10-1451-2019, 2019
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The fall of the Dead Sea level since the 1960s has provoked the formation of over 6000 sinkholes, a major hazard to local economy and infrastructure. In this context, we study the evolution of subsidence phenomena at three area scales at the Dead Sea’s eastern shore from 1967–2017. Our results yield the most detailed insights to date into the spatio-temporal development of sinkholes and larger depressions (uvalas) in an evaporite karst setting and emphasize a link to the falling Dead Sea level.
Djamil Al-Halbouni, Eoghan P. Holohan, Abbas Taheri, Robert A. Watson, Ulrich Polom, Martin P. J. Schöpfer, Sacha Emam, and Torsten Dahm
Solid Earth, 10, 1219–1241, https://doi.org/10.5194/se-10-1219-2019, https://doi.org/10.5194/se-10-1219-2019, 2019
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A 2-D numerical modelling approach to simulate the mechanical formation of sinkhole cluster inside large-scale karstic depressions is presented. Different multiple cavity growth scenarios at depth are compared regarding the mechanical process and collapse style. The outcomes of the models are compared to results from remote sensing and geophysics for an active sinkhole area in the Dead Sea region.
Michael Hodge, Juliet Biggs, Åke Fagereng, Austin Elliott, Hassan Mdala, and Felix Mphepo
Solid Earth, 10, 27–57, https://doi.org/10.5194/se-10-27-2019, https://doi.org/10.5194/se-10-27-2019, 2019
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This work attempts to create a semi-automated algorithm (called SPARTA) to calculate height, width and slope of surface breaks produced by earthquakes on faults. We developed the Python algorithm using synthetic catalogues, which can include noise features such as vegetation, hills and ditches, which mimic natural environments. We then apply the algorithm to four fault scarps in southern Malawi, at the southern end of the East African Rift system, to understand their earthquake potential.
Bruno Cagnoli and Antonio Piersanti
Solid Earth, 8, 177–188, https://doi.org/10.5194/se-8-177-2017, https://doi.org/10.5194/se-8-177-2017, 2017
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The purpose of our research is to understand the mechanisms that determine the mobility of granular flows of rock fragments. Since rock avalanches and pyroclastic flows are too dangerous to be studied at close range, we use numerical simulations and laboratory experiments. We focus on the fundamentals upon which new numerical models will be built to predict the behaviors of natural flows. These fundamentals include the effects of grain size, flow volume and channel width.
Alexis Nutz and Mathieu Schuster
Solid Earth, 7, 1609–1618, https://doi.org/10.5194/se-7-1609-2016, https://doi.org/10.5194/se-7-1609-2016, 2016
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From the geomorphology of a palaeodelta complex of Lake Turkana (Kenya), we explore the end of the Holocene African Humid Period (AHP) that corresponded to a major change in climate of Africa and that had important environmental impacts. Here, we propose that the transition from a wet to a dry period at the end of the AHP is stepwise, discussing a potential control by short-term variations in solar activity. Understanding this climate event is crucial to facing future climate changes.
Enric Vázquez-Suñé, Miguel Ángel Marazuela, Violeta Velasco, Marc Diviu, Andrés Pérez-Estaún, and Joaquina Álvarez-Marrón
Solid Earth, 7, 1317–1329, https://doi.org/10.5194/se-7-1317-2016, https://doi.org/10.5194/se-7-1317-2016, 2016
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This study shows the need for a symbiotic relationship between government and research groups for efficient management of geologic data in urban environments. Through its implementation, both the city administration and private companies benefit from the feedback of geologic knowledge acquired during this process, thereby substantially reducing the cost of construction projects and facilitating the development of aquifer management plans.
Abdulvahed Khaledi Darvishan, Vafa Homayounfar, and Seyed Hamidreza Sadeghi
Solid Earth, 7, 1293–1302, https://doi.org/10.5194/se-7-1293-2016, https://doi.org/10.5194/se-7-1293-2016, 2016
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Different stages of soil removal, transfer, preparation and placement in laboratory plots cause significant changes in soil structure and, subsequently, the results of runoff, sediment concentration and soil loss. The increasing rates of runoff coefficient, sediment concentration and soil loss due to the study soil preparation method for laboratory soil erosion plots were 179, 183 and 1050 % (2.79, 2.83 and 11.50 times), respectively.
Jozef Gallik and Lenka Bolešová
Solid Earth, 7, 1033–1042, https://doi.org/10.5194/se-7-1033-2016, https://doi.org/10.5194/se-7-1033-2016, 2016
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Technology is moving ahead very fast, and so researchers have new possibilities for their research. We tried to demonstrate benefits of using remote-sensing technology (Phantom 1 drone) such as its accuracy in the terrain, easy access to hardly accessible areas, and the possibility to collect data even during unfavourable weather conditions. The high mountainous environment provided us great conditions for testing the drone as a device for very easy and accurate mapping of natural phenomena.
Mohammad Hassan Sadeghravesh, Hassan Khosravi, and Soudeh Ghasemian
Solid Earth, 7, 673–683, https://doi.org/10.5194/se-7-673-2016, https://doi.org/10.5194/se-7-673-2016, 2016
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Select appropriate strategies according to all effective criteria in combating desertification process can be so useful in controlling and rehabilitation of degraded lands, and avoid degradation in vulnerable fields. This study provides systematic and optimal strategies of combating desertification by group decision-making model. To this end, in the framework of Multi Attribute Decision Making (MADM) and by using Delphi model (Delphi), the preferences of indexes were obtained.
Guang Jie Luo, Shi Jie Wang, Xiao Yong Bai, Xiu Ming Liu, and An Yun Cheng
Solid Earth, 7, 457–468, https://doi.org/10.5194/se-7-457-2016, https://doi.org/10.5194/se-7-457-2016, 2016
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For accurately reflecting the eco-hydrological process of the dual structure of the surface and subsurface, we propose a new method for the extraction of small watersheds in karst regions. In this study, we think that the minimum karst watershed has an exit at the corrosion–erosion datum, and the further karst sub-watershed division may cause an eco-hydrological fault. The watersheds delineated by our method accurately reflect the hydrological process in the Sancha River.
J. Rodrigo Comino, C. Brings, T. Lassu, T. Iserloh, J. M. Senciales, J. F. Martínez Murillo, J. D. Ruiz Sinoga, M. Seeger, and J. B. Ries
Solid Earth, 6, 823–837, https://doi.org/10.5194/se-6-823-2015, https://doi.org/10.5194/se-6-823-2015, 2015
M. Arian and Z. Aram
Solid Earth, 5, 1277–1291, https://doi.org/10.5194/se-5-1277-2014, https://doi.org/10.5194/se-5-1277-2014, 2014
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The Kermanshah area in the High Zagros, Iran (the collision of the Arabian and Eurasian plates) has been affected by four classes of tectonic variation. These regions were identified as very high, high, moderate and low relative tectonic activity by calculation and analysis of six geomorphic indices.
A. Gómez-Ortiz, M. Oliva, F. Salvador-Franch, M. Salvà-Catarineu, D. Palacios, J. J. de Sanjosé-Blasco, L. M. Tanarro-García, J. Galindo-Zaldívar, and C. Sanz de Galdeano
Solid Earth, 5, 979–993, https://doi.org/10.5194/se-5-979-2014, https://doi.org/10.5194/se-5-979-2014, 2014
R. Sutinen, I. Aro, P. Närhi, M. Piekkari, and M. Middleton
Solid Earth, 5, 683–691, https://doi.org/10.5194/se-5-683-2014, https://doi.org/10.5194/se-5-683-2014, 2014
Y. Liu, F. Métivier, J. Gaillardet, B. Ye, P. Meunier, C. Narteau, E. Lajeunesse, T. Han, and L. Malverti
Solid Earth, 2, 283–301, https://doi.org/10.5194/se-2-283-2011, https://doi.org/10.5194/se-2-283-2011, 2011
H. C. Ho
Solid Earth, 2, 155–158, https://doi.org/10.5194/se-2-155-2011, https://doi.org/10.5194/se-2-155-2011, 2011
A. Limare, M. Tal, M. D. Reitz, E. Lajeunesse, and F. Métivier
Solid Earth, 2, 143–154, https://doi.org/10.5194/se-2-143-2011, https://doi.org/10.5194/se-2-143-2011, 2011
Cited articles
Allen, C. E., Darmody, R. G., Thorn, C. E., Dixon, J. C., and Schlyster, P.: Clay mineralogy, chemical weathering and landscape evolution in Artic-Alpine Sweden, Geoderma, 99, 277–294, 2001.
Birks, H. H.: Holocene vegetational history and climatic change in west Spitsbergen – plant macrofossils from Skardtjørna, an Arctic lake, Holocene, 1, 209–218, 1991.
Bokhorst, M. P., Beets, C. J., Markovic, S. B., Gerasimenko, N. P., Matviishina, Z. N., and Frenchen, M.: Pedo-chemical climate proxies in Late Pleistocene Serbian-Ukrainian loess sequences, Quatern. Int., 198, 113–123, 2009.
Bryant, Y. D.: Loess deposits in Lower Adventdalen, Spitsbergen, Polar Res, 2, 93–103, 1982.
Burn, C. R.: Implications for paleoenvironmental reconstruction of recent ice-wedge development at Mayo, Yukon territory, Permafrost Periglac., 1, 3–14, 1990.
Christiansen, H. H.: Thermal regime of ice-wedge cracking in Adventdalen, Svalbard, Permafrost Periglac., 16, 87–98, 2005.
Christiansen, H. H. and Humlum, O.: Interannual variations in active layer thickness in Svalbard, Proceedings of the Ninth International Conference on Permafrost, University of Alaska, Institute of Northern Engineering Fairbanks, USA, 257–262, 2008.
Christiansen, H. H., Etzelmüller, B., Isaksen, K., Juliussen, H., Farbrot, H., Humlum, O., Johansson, M., Ingeman-Nielsen, T., Kristensen, L., Hjort, J., Holmlund, P., Sannel, A., Sigsgaard, C., Åkerman, H. J., Foged, N., Blikra, L., Pernosky, M. A., and Ødegård, R. S.: The thermal state of permafrost in the Nordic area during the International Polar Year 2007–2009, Permafrost Periglac., 21, 156–181, 2010.
Daviel, A., Sanborn, P., Tarnocai, C., and Smith, C. A.: Clay mineralogy and chemical properties of argilic horizons in central Yukon paleosols, Can. J. Soil. Sci., 91, 83–93, 2011.
Divine, D., Isaksson, E., Martma, T., Meijer, H. A., Moore, J., Pohjola, V., van de Wal, R. S., and Godtliebsen, F.: Thousand years of winter surface air temperature variations in Svalbard and northern Norway reconstructed from ice-core data, Polar Res., 30, 73–79, 2011.
Drewnik, M., Skiba, M., Szymanski, W., and Zyla, M.: Mineral composition vs. soil forming in loess soils – a case study from Krakow (Southern Poland), Catena, https://doi.org/10.1016/j.catena.2014.02.012, 2014.
Egli, M., Dahms, D., and Norton, K.: Soil formation rates on silicate parent material in alpine environments: Different approaches – different results?, Geoderma, 213, 320–333, 2014.
Ellis, C. J. and Rochefort, L.: Long-term sensitivity of a High Arctic wetland to Holocene climate change, J. Ecol., 94, 441–454, 2006.
Finke, P. A.: Modelling the genesis of livisols as a function of topographic position in loess material, Quatern. Int., 265, 3–17, 2012.
Finke, P. A., Vanwalleghem, T., Opolot, E., Poesen, J., and Deckers, S.: Estimating the effect of tree uprooting on variation of soil horizon depth by confronting pedogenetic simulations to measurements in a Belgian loess area, J. Geophys. Res., 118, 1–16, 2013.
Førland, E. J., Rasmus, B., Hanssen-Bauer, I., Haugen, J. E., and Skaugen, T. E.: Temperature and precipitation development at Svalbard 1900–2100, Adv. Meteorol., 893790, https://doi.org/10.1155/2011/893790, 2011.
Fortier, D. and Allard, M.: Late Holocene syngenetic ice-wedge polygons development, Bylot Island, Canadian Arctic Archipelago, Can. J. Earth. Sci., 41, 997–1012, 2004.
Fortier, D. and Allard, M.: Frost-cracking conditions, Bylot Island, eastern Canadian Arctic archipelago, Permafrost Periglac., 16, 145–161, 2005.
Fortier, D., Allard, M., and Pivot, F.: A late-Holocene record of loess deposition in ice-wedge polygons reflecting wind activity and ground moisture conditions, Bylot Island, eastern Canadian Arctic, Holocene, 16, 635–646, 2006.
Forwick, M. and Vorren, T. O.: Stratigraphy and deglaciation of the Isfjorden area, Spitsbergen, Norw. J. Geol., 90, 163–179, 2010.
French, H.: The periglacial environment, Wiley, West Sussex, England, Third Edition, 2007.
Gallet, S., Jahn, B., Van Vliet-Lanoë, B., Dia, A., and Rosello, E.: Loess geochemistry and its implications for particle origin and composition of the upper continental crust, Earth Planet. Sc. Lett., 156, 157–172, 1998.
Galovic, L., Frechen, M., Peh, Z., Durn., and Halamic, J.: Loess/palaeosol section in Sarengrad, Croatia – a qualitative discussion on the correlation of geochemical and magnetic susceptibility data, Quatern. Int., 240, 22–34, 2011.
Grinsted, A., Moore, J. C., Pohjola, V., Martma, T., and Isaksson, E.: Svalbard summer melting, continentality, and sea ice extent from the Lomonosovfonna ice core, J. Geophys. Res., 111, https://doi.org/10.1029/2005JD006494, 2006.
Hagen, J. O., Liestøl, O., Roland, E., and Jørgensen, T.: Glacier atlas of Svalbard and Jan Mayen, Norsk Polarinst, Map 129, 1993.
Hald, M., Dahlgren, T., Olsen, T., and Lebesbye, E.: Late Holocene palaeoceanography in Van Mijenfjorden, Svalbard, Polar Res., 20, 23–35, 2001.
Hall, K., Thorn, C. E., Matsuoka, N., and Prick, A.: Weathering in cold regions: some thoughts and perspectives, Prog. Phys. Geog., 26, 577–603, 2002.
Hall, K.: Rock temperatures and implications for cold region weathering. I: New data from Viking valley, Alexander Island, Antarctica, Permafrost Periglac., 8, 69–90, 1997.
Hall, K.: Evidence for freeze-thaw events and their implications for rock weathering in Northern Canada, Earth. Surf. Proc. Land., 29, 43–57, 2004.
Härtel, S.: Formation and dynamics of Holocene ice-wedge polygons in Lower Adventdalen, Svalbard, M. S. thesis, University of Svalbard, Norway, 114 pp., 2011.
Holmgren, S., Bigler, C., Ingolfsson, O., and Wolfe, A. P.: The Holocene-Anthropocene transition in lakes of western Spitsbergen, Svalbard (Norwegian High Arctic): Climate change and nitrogen deposition, J. Paleolimnol., 43, 393–412, 2010.
Huang, C. Q., Zhao, W., Li, F. Y., Tan, W. F., and Wang, M. K.: Mineralogical and pedogenetic evidence for paleoenvironmental variations during the Holocene on the Loess Plateau, China, Catena, 96, 49–56, 2012.
Humlum, O.: Holocene permafrost aggradation in Svalbard. Geological Society of London Special Publication, 242, 119–129, 2005.
Humlum, O., Instanes, A., and Sollid, J.L.: Permafrost in Svalbard: a review of research history, climatic background and engineering challenges, Polar Res, 22, 191–215, 2003.
Humlum, O., Elberling, B., Hormes, A., Fjordheim, K., Hansen, O. H., and Heinemeier, J.: Late-Holocene glacier growth in Svalbard, documented by subglacial relict vegetation and living soil microbes, Holocene, 15, 396–407, 2005.
Humlum, O., Solheim, J. E., and Stordahl, K.: Spectral analysis of the Svalbard temperature record 1912–2010, Advances in Meteorology, 175296, https://doi.org/10.1155/2011/175296, 2011a.
Humlum, H., Solheim,, J. E., and Stordahl, K.:. Identifying natural contributions to late Holocene climate change, Global Planet. Change, 79, 145–156, 2011b.
Isaksson, E., Divine D., Kohler, J., Martma, T., Pohjola, V., Motoyama, H., and Watanabe, O.: Climate oscillations as recorded in Svalbard ice core δ18O records between AD 1200 and 1997, Geogr. Ann. A., 87, 203–214, 2005.
Jackson, M. G., Oskarsson, N., Trønnes, R. G., McManus, J. F., Oppo, D. W., Grönvold, K., Stanley R. Hart, S. R., and Sachs, J. P.: Holocene loess deposition in Iceland: Evidence for millennial-scale atmosphere-ocean coupling in the North Atlantic, Geology, 33, 509–512, 2005.
Jahn, B. M., Gallet, S., and Han, J.: Geochemistry of the Xining, Xifeng and Jixian sections, Loess Plateau of China: eolian dust provenance and paleosol evolution during the last 140 ka, Chem. Geol., 178, 71–94, 2001.
Jeppesen, J. W.: Ice wedges and host sediments as palaeoclimatic indicators in central Spitsbergen, Svalbard (in Danish), M.S. thesis, University of Copenhagen, Denmark, 101 pp., 2001.
Jonassen, M. O., Olafsson, H., Reuder, J., and Olseth, J. A.: Multi-scale variability winds in the complex topography of southwestern Norway, Tellus, 64, 11962, https://doi.org/10.3402/tellusa.v64i0.11962, 2012.
Kempf, P., Forwick, M., Laberg, J. S., and Vorren, T. O.: Late Weichselian – Holocene sedimentary palaeoenvironment and glacial activity in the high-Arctic van Keulenfjorden, Spitsbergen, Holocene, 23, 1605–1616, 2013.
Lachenbruch, A. H.: Mechanics of thermal contraction cracks and ice-wedge polygons in permafrost, Geol. Soc. Am., 70, 1–68, 1962.
Liestøl, O.: Pingos, springs and permafrost in Spitsbergen, Norsk Polarinst. Skri., 1975, 7–29, 1976.
Liestøl, O.: The glaciers in the Kongsfjorden area, Spitsbergen, Norsk Geogr. Tidsskr., 42, 231–238, 1988.
Lønne, I. and Lyså, A.: Deglaciation dynamics following the Little Ice Age on Svalbard: implications for shaping of landscapes at high latitudes, Geomorphology, 72, 300–319, 2005.
Lønne, I. and Nemec, W.: High-arctic fan delta recording deglaciation and environmental disequilibrium, Sedimentology, 51, 553–589, 2004.
Mackay, J. R.: Thermally induced movements in ice-wedge polygons, western arctic coast: a long-terms study, Geogr. Phys. Quatern., 54, 41–68, 2000.
Major, H., Haremo, P., Dallmann, W. K., and Andresen, A.: Geological Map of Svalbard 1, 100,000, Norsk Polarinst, Map C9G Adventdalen, 31–32, 2001.
Matsuoka, N. and Murton, J.: Frost weathering: recent advances and future directions, Permafrost Periglac., 19, 195–210, 2008.
Moberg, A., Sonechkin, D. M., Holmgren, K., Datsenko, N. M., and Karlenm, W.: Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data, Nature, 433, 613–617, 2005.
Moros, M., Jansen, E., Oppo, D.W., Giraudeau, J., and Kuijpers, A.: Reconstruction of the late-Holocene changes in the Sub-Arctic Front position at the Reykjanes Ridge, north Atlantic, Holocene, 22, 877–886, 2012.
Nesbitt, H. W., and Young, G. M.: Early Proterozoic climates and plate montions inferred from major element chemistry of lutites, Nature, 229, 715–717, 1982.
Opel, T., Dereviagin, A. Yu., Meyer, H., Schirrmeister, L., and Wetterich, S.: Palaeoclimatic information from stable water isotopes of Holocene ice wedges on the Dmitrii Laptev Strait, northeast Siberia, Russia, Permafrost Periglac., 22, 84–100, 2011.
Pina, P.: Polygonal pattern analysis on Mars based on Svalbard analogues, Proceedings of the V Iberian Conference of the International Permafrost Association, University of Barcelona, in press, 2014.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Bronk Ramsey, C., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P. M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatté, C., Heaton, T. J., Hoffmann, D. L., Hogg, A., Hughen, K. A., Kaiser, K. F., Kromer, B., Manning, S. W., Niu, M., Reimer, R. W., Richards, D. A., Scott, E. M., Southon, J. R., Staff, R. A., Turney, C. S. M., and van der Plicht, J.: IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP, Radiocarbon, 55, 1869–1887, 2013.
Salvigsen, O.: Radiocarbon-dated Mytilus edulis and Modiolus modiolus from northern Svalbard: climatic implications, Norsk Geogr Tidsskr, 56, 56–61, 2002.
Salvigsen, O., Forman, S. L., and Miller, G. H.: Thermophilous molluscs on Svalbard during the Holocene and their paleoclimatic implications, Polar Res., 11, 1–10, 1992.
Saraiva, J., Lousada, M., Pina, P., Bandeira, L., and Vieira, G.: Geometric and topologic characterization of periglacial polygonal networks in Adventdalen, Svalbard, Norway, EGU General Assembly, Vienna, Austria, 22–27 April 2012, EGU2012-10818-1, 2012.
Schwamborn, G., Meyer, H., Fedorov, G., Schirrmeister, L., and Hubberten, H. W.: Ground ice and slope sediments archiving Late Quaternary paleoenvironment and paleoclimate signals at the margins of Elgygytgyn Crater, NE Siberia, Quaternary Res., 66, 259–272, 2006.
Skirbekk, K., Klitgaard-Kristensen, D., Rasmussen, T. L., Koç, N., and Forwick., M.: Holocene climate variations at the entrance to a warm Arctic fjord: evidence from Kongsfjorden trough, Svalbard, in: Fjordic Depositional Systems and Archives, Geological Society of London Special Publication, 344, 289–304, 2010.
Snyder, J. A., Werner, A., and Miller, G. H.: Holocene cirque glacier activity in western Spitsbergen, Svalbard: sediment records from proglacial Linnévatnet, Holocene, 10, 555–563, 2000.
Sørbel L. and Tolgensbakk, J.: Ice-wedge polygons and solifluction in the Adventdalen area, Spitsbergen, Svalbard, Norsk Geogr. Tidsskr., 56, 62–66, 2002.
Svendsen, J. I. and Mangerud, J.: Holocene glacial and climatic variations on Spitsbergen, Svalbard, Holocene 7, 45–57, 1997.
Sun, J. M. and Liu, T.: Multiple origins and interpretations of magnetic susceptibility signal in Chinese wind-blow sediments, Earth Planet. Sc. Lett., 180, 287–296, 2000.
Sundqvist, H. S., Zhang, Q., Moberg, A., Holmgren, K., Körnich, H., Nilsson, J., and Brattström, G.: Climate change between the mid and late Holocene in northern high latitudes – Part 1: Survey of temperature and precipitation proxy data, Clim. Past, 6, 591–608, https://doi.org/10.5194/cp-6-591-2010, 2010.
Thorn, C. E., Darmody, R. G., Dixon, J. C., and Schlyter, P.: The chemical weathering regime of Karkevagge, arctic-alpine Sweden, Geomorphology, 41, 37–52, 2001.
Ulrich, M., Hauber, E., Herzschuh, U., Härtel, S., and Schirrmeister, L.: Polygon pattern geomorphometry on Svalbard (Norway) and western Utopia Planitia (Mars) using high-resolution stereo remote-sensing data, Geomorphology, 134, 197–216, 2011.
\'Ujvári, G., Varga, A., and Balogh-Brunstad, Z.: Origin, weathering, and geochemical 20 composition of loess in southwestern Hungary, Quaternary Res., 69, 421–437, 2008.
Vandenberghe, J.: Grain size of fine-grained windblow sediment: a powerfull proxy for process indentification, Earth. Sci. Rev, 121, 18–30, 2013.
Varga, A., Ujvari, G., and Raucsik, B.: Tectonic vs. climatic control on the evolution of a loess-paleosol sequence at Bermend, Hungary: an integrated approach based on paleoecological, clay mineralogical, and geochemical data, Quatern. Int., 240, 71–86, 2011.
Velle, J. H.: Holocene sedimentary environments in Smeerenburgfjorden, Spitsbergen, M.S. thesis, University of Tromsø, Norway, 128 pp., 2012.
Vinther, B. M., Clausen, H. B., Johnsen, S. J., Rasmussen, S. O., Andersen, K. K., Buchardt, S. L., Dahl Jensen, D., Seierstad, I. K., Siggaard-Andersen, M. L., Steffensen, J. P., Svensson, A., Olsen, J., and Heinemeier, J.: A synchronized dating of three Greenland ice cores throughout the Holocene, J. Geophys. Res., 111, D13102, https://doi.org/10.1029/2005JD006921, 2006.
Wanner, H., Beer, J., Butikofer, J., Crowley, T.J., Cubasch, U., Fluckiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J. O., Kuttel, M., Muller, S. A., Prentice, I. C., Solomina, O., Stocker, T. F., Tarasov, P., Wagner, M., and Widmann, M.: Mid-to Late Holocene climate change: an overview, Quaternary Sci. Rev., 27, 1791–1828, 2008.
Watanabe, T., Matsuoka, N., and Christiansen, H. H.: Mudboil and ice-wedge dynamics investigated by electrical resistivity tomography, ground temperatures and surface movements in Svalbard, Geogr. Ann. A., 94, 445–457, 2012a.
Watanabe, T., Matsuoka, N., and Christiansen, H. H.: Controls on patterned ground variability at a continuous permafrost site, central Spitsbergen, Proceedings of the Tenth International Conference on Permafrost, 1, 433–438, 2012b.
Watanabe, T., Matsuoka, N., and Christiansen, H. H.: Ice- and soil-wedge dynamics in the Kapp Linné Area, Svalbard, investigated by two- and three-dimensional GPR and ground thermal and acceleration regimes, Permafrost Periglac., 24, 39–55, 2013.
Zech, M., Zech, R., Zech, W., Glaser, B., Brodowski, S., and Amelung, W.: Characterisation and paleoclimate of a loess-like permafrost paleosol sequence in NE Siberia, Geoderma, 143, 281–295, 2008.
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