Articles | Volume 14, issue 3
https://doi.org/10.5194/essd-14-1043-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-14-1043-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Data description paper
| 
09 Mar 2022
Data description paper |
| 09 Mar 2022
| 09 Mar 2022
An hourly ground temperature dataset for 16 high-elevation sites (3493–4377 m a.s.l.) in the Bale Mountains, Ethiopia (2017–2020)
Alexander R. Groos
CORRESPONDING AUTHOR
Institute of Geography, University of Bern, 3012 Bern, Switzerland
Institute of Geography, Friedrich-Alexander-Universität Erlangen-Nürnberg, 91508 Erlangen, Germany
Janik Niederhauser
Institute of Geography, University of Bern, 3012 Bern, Switzerland
Bruk Lemma
Institute of Agronomy and Nutritional Sciences, Martin Luther University Halle-Wittenberg, 06120 Halle, Germany
Forest and Rangeland Biodiversity Directorate, Ethiopian Biodiversity Institute, P.O. Box 30726, Addis Ababa, Ethiopia
Mekbib Fekadu
Department of Geography, Philipps University of Marburg, 35032 Marburg, Germany
Department of Plant Biology and Biodiversity Management, Addis Ababa University, P.O. Box 3434, Addis Ababa, Ethiopia
Wolfgang Zech
Soil Science Department, University of Bayreuth, 95440 Bayreuth, Germany
Falk Hänsel
Department of Geography, Philipps University of Marburg, 35032 Marburg, Germany
Luise Wraase
Department of Geography, Philipps University of Marburg, 35032 Marburg, Germany
Naki Akçar
Institute of Geological Sciences, University of Bern, 3012 Bern, Switzerland
Heinz Veit
Institute of Geography, University of Bern, 3012 Bern, Switzerland
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The lower part of mountain glaciers is often covered with debris. Knowing the thickness of the debris is important as it influences the melting and future evolution of the affected glaciers. We have developed an open-source approach to map variations in debris thickness on glaciers using a low-cost drone equipped with a thermal infrared camera. The resulting high-resolution maps of debris surface temperature and thickness enable more accurate monitoring and modelling of debris-covered glaciers.
Alexander R. Groos, Janik Niederhauser, Luise Wraase, Falk Hänsel, Thomas Nauss, Naki Akçar, and Heinz Veit
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Large sorted stone stripes have been discovered on the 4000 m high central Sanetti Plateau of the tropical Bale Mountains in Ethiopia. The stripes are a mystery as similar landforms have so far only been reported in the temperate zone and polar regions. Our investigations suggest that the stripes formed in the vicinity of a former ice cap on the plateau during a much colder climatic period. The distinct pattern is the result of a process related to cyclic freezing and thawing of the ground.
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The lower part of mountain glaciers is often covered with debris. Knowing the thickness of the debris is important as it influences the melting and future evolution of the affected glaciers. We have developed an open-source approach to map variations in debris thickness on glaciers using a low-cost drone equipped with a thermal infrared camera. The resulting high-resolution maps of debris surface temperature and thickness enable more accurate monitoring and modelling of debris-covered glaciers.
Elena Serra, Pierre G. Valla, Romain Delunel, Natacha Gribenski, Marcus Christl, and Naki Akçar
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Alpine landscapes are transformed by several erosion processes. 10Be concentrations measured in river sediments at the outlet of a basin represent a powerful tool to quantify how fast the catchment erodes. We measured erosion rates within the Dora Baltea catchments (western Italian Alps). Our results show that erosion is governed by topography, bedrock resistance and glacial imprint. The Mont Blanc massif has the highest erosion and therefore dominates the sediment flux of the Dora Baltea river.
Irene Schimmelpfennig, Joerg M. Schaefer, Jennifer Lamp, Vincent Godard, Roseanne Schwartz, Edouard Bard, Thibaut Tuna, Naki Akçar, Christian Schlüchter, Susan Zimmerman, and ASTER Team
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Small mountain glaciers advance and recede as a response to summer temperature changes. Dating of glacial landforms with cosmogenic nuclides allowed us to reconstruct the advance and retreat history of an Alpine glacier throughout the past ~ 11 000 years, the Holocene. The results contribute knowledge to the debate of Holocene climate evolution, indicating that during most of this warm period, summer temperatures were similar to or warmer than in modern times.
Alexander R. Groos, Janik Niederhauser, Luise Wraase, Falk Hänsel, Thomas Nauss, Naki Akçar, and Heinz Veit
Earth Surf. Dynam., 9, 145–166, https://doi.org/10.5194/esurf-9-145-2021, https://doi.org/10.5194/esurf-9-145-2021, 2021
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Large sorted stone stripes have been discovered on the 4000 m high central Sanetti Plateau of the tropical Bale Mountains in Ethiopia. The stripes are a mystery as similar landforms have so far only been reported in the temperate zone and polar regions. Our investigations suggest that the stripes formed in the vicinity of a former ice cap on the plateau during a much colder climatic period. The distinct pattern is the result of a process related to cyclic freezing and thawing of the ground.
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E&G Quaternary Sci. J., 68, 189–200, https://doi.org/10.5194/egqsj-68-189-2019, https://doi.org/10.5194/egqsj-68-189-2019, 2019
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Chemotaxonomic identification of keystone plant species in the Bale Mountains are possible using lignin phenols. However, Erica could not be differentiated chemotaxonomically from all other investigated plants using n-alkanes. Unambiguous characteristic patterns of lignin phenols reflected in the plant samples were not sustained in the organic layers and mineral topsoils. This is due to degradation and organic matter inputs by roots. Therefore, the past extent of Erica is still speculative.
Betelhem Mekonnen, Wolfgang Zech, Bruno Glaser, Bruk Lemma, Tobias Bromm, Sileshi Nemomissa, Tamrat Bekele, and Michael Zech
E&G Quaternary Sci. J., 68, 177–188, https://doi.org/10.5194/egqsj-68-177-2019, https://doi.org/10.5194/egqsj-68-177-2019, 2019
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The study evaluates the ability of stable isotopes (δ13C and δ15N) and sugar biomarkers to distinguish Erica from the dominant vegetation of the Bale Mountains in order to reconstruct the past extent of Erica on the Sanetti Plateau. No significant differences in stable isotopes are found between the dominant plant species. Although Erica is characterized by quite high (G+M)/(A+X) ratios, it cannot be unambiguously distinguished from other plants due to degradation and soil microbial effects.
Lorenz Wüthrich, Claudio Brändli, Régis Braucher, Heinz Veit, Negar Haghipour, Carla Terrizzano, Marcus Christl, Christian Gnägi, and Roland Zech
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It provides a new interpretation for pre-Columbian management of raised fields.
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A 2600-year long composite palaeoflood record is reconstructed from high-resolution delta plain sediments of the Hasli-Aare floodplain on the northern slope of the Swiss Alps. Natural proxies compiled from sedimentary, geochemical and geomorphological data were calibrated by textual and factual sources and instrumental data. Geomorphological, historical and instrumental data provide evidence for flood damage intensities and discharge estimations of severe and catastrophic historical floods.
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Revised manuscript accepted for ESSD
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Tianyu Yue, Shuiqing Yin, Yun Xie, Bofu Yu, and Baoyuan Liu
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David Olefeldt, Mikael Hovemyr, McKenzie A. Kuhn, David Bastviken, Theodore J. Bohn, John Connolly, Patrick Crill, Eugénie S. Euskirchen, Sarah A. Finkelstein, Hélène Genet, Guido Grosse, Lorna I. Harris, Liam Heffernan, Manuel Helbig, Gustaf Hugelius, Ryan Hutchins, Sari Juutinen, Mark J. Lara, Avni Malhotra, Kristen Manies, A. David McGuire, Susan M. Natali, Jonathan A. O'Donnell, Frans-Jan W. Parmentier, Aleksi Räsänen, Christina Schädel, Oliver Sonnentag, Maria Strack, Suzanne E. Tank, Claire Treat, Ruth K. Varner, Tarmo Virtanen, Rebecca K. Warren, and Jennifer D. Watts
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Wetlands, lakes, and rivers are important sources of the greenhouse gas methane to the atmosphere. To understand current and future methane emissions from northern regions, we need maps that show the extent and distribution of specific types of wetlands, lakes, and rivers. The Boreal–Arctic Wetland and Lake Dataset (BAWLD) provides maps of five wetland types, seven lake types, and three river types for northern regions and will improve our ability to predict future methane emissions.
Mengna Li, Yijian Zeng, Maciek W. Lubczynski, Jean Roy, Lianyu Yu, Hui Qian, Zhenyu Li, Jie Chen, Lei Han, Han Zheng, Tom Veldkamp, Jeroen M. Schoorl, Harrie-Jan Hendricks Franssen, Kai Hou, Qiying Zhang, Panpan Xu, Fan Li, Kai Lu, Yulin Li, and Zhongbo Su
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The Tibetan Plateau is the source of most of Asia's major rivers and has been called the Asian Water Tower. Due to its remoteness and the harsh environment, there is a lack of field survey data to investigate its hydrogeology. Borehole core lithology analysis, an altitude survey, soil thickness measurement, hydrogeological surveys, and hydrogeophysical surveys were conducted in the Maqu catchment within the Yellow River source region to improve a full–picture understanding of the water cycle.
Olivier Evrard, Caroline Chartin, J. Patrick Laceby, Yuichi Onda, Yoshifumi Wakiyama, Atsushi Nakao, Olivier Cerdan, Hugo Lepage, Hugo Jaegler, Rosalie Vandromme, Irène Lefèvre, and Philippe Bonté
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This dataset provides an original compilation of radioactive dose rates and artificial radionuclide activities in sediment deposited after floods in the rivers draining the main radioactive pollution plume in Fukushuma, Japan, between November
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Qiang Zhang, Qiangqiang Yuan, Jie Li, Yuan Wang, Fujun Sun, and Liangpei Zhang
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Acquired daily soil moisture products are always incomplete globally (just about 30 %–80 % coverage ratio) due to the satellite orbit coverage and the limitations of soil moisture retrieval algorithms. To solve this inevitable problem, we generate long-term seamless global daily (SGD) AMSR2 soil moisture productions from 2013 to 2019. These productions are significant for full-coverage global daily hydrologic monitoring, rather than averaging as the monthly–quarter–yearly results.
Alexander Kmoch, Arno Kanal, Alar Astover, Ain Kull, Holger Virro, Aveliina Helm, Meelis Pärtel, Ivika Ostonen, and Evelyn Uuemaa
Earth Syst. Sci. Data, 13, 83–97, https://doi.org/10.5194/essd-13-83-2021, https://doi.org/10.5194/essd-13-83-2021, 2021
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The Soil Map of Estonia is the most detailed and information-rich dataset for soils in Estonia. But its information is not immediately usable for analyses or modelling. We derived parameters including soil layering, soil texture (clay, silt, and sand content), coarse fragments, and rock content and aggregated and predicted physical variables related to water and carbon cycles (bulk density, hydraulic conductivity, organic carbon content, available water capacity).
Yongzhe Chen, Xiaoming Feng, and Bojie Fu
Earth Syst. Sci. Data, 13, 1–31, https://doi.org/10.5194/essd-13-1-2021, https://doi.org/10.5194/essd-13-1-2021, 2021
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Soil moisture can greatly influence the ecosystem but is hard to monitor at the global scale. By calibrating and combining 11 different products derived from satellite observation, we developed a new global surface soil moisture dataset spanning from 2003 to 2018 with high accuracy. Using this new dataset, not only can the global long-term trends be derived, but also the seasonal variation and spatial distribution of surface soil moisture at different latitudes can be better studied.
Xavier Morel, Birger Hansen, Christine Delire, Per Ambus, Mikhail Mastepanov, and Bertrand Decharme
Earth Syst. Sci. Data, 12, 2365–2380, https://doi.org/10.5194/essd-12-2365-2020, https://doi.org/10.5194/essd-12-2365-2020, 2020
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Nuuk fen site is a well-instrumented Greenlandic site where soil physical variables and greenhouse gas fluxes are monitored. But knowledge of soil carbon stocks and profiles is missing. This is a crucial shortcoming for a complete evaluation of models. For the first time we measured soil carbon and nitrogen density, profiles, and stocks in the Nuuk peatland. This new dataset can contribute to further develop joint modeling of greenhouse gas emissions and soil carbon in land-surface models.
Valery Kashparov, Sviatoslav Levchuk, Marina Zhurba, Valentyn Protsak, Nicholas A. Beresford, and Jacqueline S. Chaplow
Earth Syst. Sci. Data, 12, 1861–1875, https://doi.org/10.5194/essd-12-1861-2020, https://doi.org/10.5194/essd-12-1861-2020, 2020
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Sampling and analysis methodology and spatial radionuclide deposition data from the 60 km area around the Chernobyl Nuclear Power Plant, sampled in 1987 by the Ukrainian Institute of Agricultural Radiology, are useful for reconstructing doses to human and wildlife populations, answering the current lack of scientific consensus on the effects of radiation on wildlife in the Chernobyl Exclusion Zone and evaluating future management options for the Chernobyl-impacted areas of Ukraine and Belarus.
Kristen Manies, Mark Waldrop, and Jennifer Harden
Earth Syst. Sci. Data, 12, 1745–1757, https://doi.org/10.5194/essd-12-1745-2020, https://doi.org/10.5194/essd-12-1745-2020, 2020
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Boreal ecosystems are unique in that their mineral soil is covered by what can be quite thick layers of organic soil. Layers within this organic soil have different bulk densities, carbon composition, and nitrogen composition. We summarize these properties by soil layer and examine if and how they are affected by soil drainage and stand age. These values can be used to initialize and validate models as well as gap fill when these important soil properties are not measured.
Conrad Jackisch, Kai Germer, Thomas Graeff, Ines Andrä, Katrin Schulz, Marcus Schiedung, Jaqueline Haller-Jans, Jonas Schneider, Julia Jaquemotte, Philipp Helmer, Leander Lotz, Andreas Bauer, Irene Hahn, Martin Šanda, Monika Kumpan, Johann Dorner, Gerrit de Rooij, Stefan Wessel-Bothe, Lorenz Kottmann, Siegfried Schittenhelm, and Wolfgang Durner
Earth Syst. Sci. Data, 12, 683–697, https://doi.org/10.5194/essd-12-683-2020, https://doi.org/10.5194/essd-12-683-2020, 2020
Short summary
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Soil water content and matric potential are central hydrological state variables. A large variety of automated probes and sensor systems for field monitoring exist. In a field experiment under idealised conditions we compared 15 systems for soil moisture and 14 systems for matric potential. The individual records of one system agree well with the others. Most records are also plausible. However, the absolute values of the different measuring systems span a very large range of possible truths.
Marco Pfeiffer, José Padarian, Rodrigo Osorio, Nelson Bustamante, Guillermo Federico Olmedo, Mario Guevara, Felipe Aburto, Francisco Albornoz, Monica Antilén, Elías Araya, Eduardo Arellano, Maialen Barret, Juan Barrera, Pascal Boeckx, Margarita Briceño, Sally Bunning, Lea Cabrol, Manuel Casanova, Pablo Cornejo, Fabio Corradini, Gustavo Curaqueo, Sebastian Doetterl, Paola Duran, Mauricio Escudey, Angelina Espinoza, Samuel Francke, Juan Pablo Fuentes, Marcel Fuentes, Gonzalo Gajardo, Rafael García, Audrey Gallaud, Mauricio Galleguillos, Andrés Gomez, Marcela Hidalgo, Jorge Ivelic-Sáez, Lwando Mashalaba, Francisco Matus, Francisco Meza, Maria de la Luz Mora, Jorge Mora, Cristina Muñoz, Pablo Norambuena, Carolina Olivera, Carlos Ovalle, Marcelo Panichini, Aníbal Pauchard, Jorge F. Pérez-Quezada, Sergio Radic, José Ramirez, Nicolás Riveras, Germán Ruiz, Osvaldo Salazar, Iván Salgado, Oscar Seguel, Maria Sepúlveda, Carlos Sierra, Yasna Tapia, Francisco Tapia, Balfredo Toledo, José Miguel Torrico, Susana Valle, Ronald Vargas, Michael Wolff, and Erick Zagal
Earth Syst. Sci. Data, 12, 457–468, https://doi.org/10.5194/essd-12-457-2020, https://doi.org/10.5194/essd-12-457-2020, 2020
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The CHLSOC database is the biggest soil organic carbon (SOC) database that has been compiled for Chile yet, comprising 13 612 data points. This database is the product of the compilation of numerous sources including unpublished and difficult-to-access data, allowing us to fill numerous spatial gaps where no SOC estimates were publicly available before. The values of SOC compiled in CHLSOC have a wide range, reflecting the variety of ecosystems that exists in Chile.
Corey R. Lawrence, Jeffrey Beem-Miller, Alison M. Hoyt, Grey Monroe, Carlos A. Sierra, Shane Stoner, Katherine Heckman, Joseph C. Blankinship, Susan E. Crow, Gavin McNicol, Susan Trumbore, Paul A. Levine, Olga Vindušková, Katherine Todd-Brown, Craig Rasmussen, Caitlin E. Hicks Pries, Christina Schädel, Karis McFarlane, Sebastian Doetterl, Christine Hatté, Yujie He, Claire Treat, Jennifer W. Harden, Margaret S. Torn, Cristian Estop-Aragonés, Asmeret Asefaw Berhe, Marco Keiluweit, Ágatha Della Rosa Kuhnen, Erika Marin-Spiotta, Alain F. Plante, Aaron Thompson, Zheng Shi, Joshua P. Schimel, Lydia J. S. Vaughn, Sophie F. von Fromm, and Rota Wagai
Earth Syst. Sci. Data, 12, 61–76, https://doi.org/10.5194/essd-12-61-2020, https://doi.org/10.5194/essd-12-61-2020, 2020
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The International Soil Radiocarbon Database (ISRaD) is an an open-source archive of soil data focused on datasets including radiocarbon measurements. ISRaD includes data from bulk or
whole soils, distinct soil carbon pools isolated in the laboratory by a variety of soil fractionation methods, samples of soil gas or water collected interstitially from within an intact soil profile, CO2 gas isolated from laboratory soil incubations, and fluxes collected in situ from a soil surface.
Hong Zhao, Yijian Zeng, Shaoning Lv, and Zhongbo Su
Earth Syst. Sci. Data, 10, 1031–1061, https://doi.org/10.5194/essd-10-1031-2018, https://doi.org/10.5194/essd-10-1031-2018, 2018
Short summary
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The Tibet-Obs soil properties dataset was compiled based on in situ and laboratory measurements of soil profiles across three climate zones on the Tibetan Plateau. The appropriate parameterization schemes of soil hydraulic and thermal properties were discussed for their applicability in land surface modeling. The uncertainties of existing soil datasets were evaluated. This paper contributes to land surface modeling and hydro-climatology communities for their studies of the third pole region.
Valery Kashparov, Sviatoslav Levchuk, Marina Zhurba, Valentyn Protsak, Yuri Khomutinin, Nicholas A. Beresford, and Jacqueline S. Chaplow
Earth Syst. Sci. Data, 10, 339–353, https://doi.org/10.5194/essd-10-339-2018, https://doi.org/10.5194/essd-10-339-2018, 2018
Short summary
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Spatial datasets of radionuclide contamination in the Ukrainian Chernobyl Exclusion Zone describe data from analysis of samples collected by the Ukrainian Institute of Agricultural Radiology after the Chernobyl nuclear accident between May 1986 and 2014 at sites inside the Chernobyl Exclusion Zone and other areas of interest. The data and supporting documentation are freely available from the Environmental Information Data Centre: https://doi.org/10.5285/782ec845-2135-4698-8881-b38823e533bf.
Carsten Montzka, Michael Herbst, Lutz Weihermüller, Anne Verhoef, and Harry Vereecken
Earth Syst. Sci. Data, 9, 529–543, https://doi.org/10.5194/essd-9-529-2017, https://doi.org/10.5194/essd-9-529-2017, 2017
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Global climate models require adequate parameterization of soil hydraulic properties, but typical resampling to the model grid introduces uncertainties. Here we present a method to scale hydraulic parameters to individual model grids and provide a global data set that overcomes the problems. It preserves the information of sub-grid variability of the water retention curve by deriving local scaling parameters that enables modellers to perturb hydraulic parameters for model ensemble generation.
Niels H. Batjes, Eloi Ribeiro, Ad van Oostrum, Johan Leenaars, Tom Hengl, and Jorge Mendes de Jesus
Earth Syst. Sci. Data, 9, 1–14, https://doi.org/10.5194/essd-9-1-2017, https://doi.org/10.5194/essd-9-1-2017, 2017
Short summary
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Soil is an important provider of ecosystem services. Yet this natural resource is being threatened. Professionals, scientists, and decision makers require quality-assessed soil data to address issues such as food security, land degradation, and climate change. Procedures for safeguarding, standardising, and subsequently serving of consistent soil data to underpin broad-scale mapping and modelling are described. The data are freely accessible at doi:10.17027/isric-wdcsoils.20160003.
J. S. Chaplow, N. A. Beresford, and C. L. Barnett
Earth Syst. Sci. Data, 7, 215–221, https://doi.org/10.5194/essd-7-215-2015, https://doi.org/10.5194/essd-7-215-2015, 2015
Short summary
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The data set ‘Post Chernobyl surveys of radiocaesium in soil, vegetation, wildlife and fungi in Great Britain’ was developed to enable data collected by the Natural Environment Research Council after the Chernobyl accident to be made publicly available. Data for samples collected between May 1986 (immediately after Chernobyl) to spring 1997 are freely available for non-commercial use under Open Government Licence terms and conditions. doi: 10.5285/d0a6a8bf-68f0-4935-8b43-4e597c3bf251.
G. Hugelius, J. G. Bockheim, P. Camill, B. Elberling, G. Grosse, J. W. Harden, K. Johnson, T. Jorgenson, C. D. Koven, P. Kuhry, G. Michaelson, U. Mishra, J. Palmtag, C.-L. Ping, J. O'Donnell, L. Schirrmeister, E. A. G. Schuur, Y. Sheng, L. C. Smith, J. Strauss, and Z. Yu
Earth Syst. Sci. Data, 5, 393–402, https://doi.org/10.5194/essd-5-393-2013, https://doi.org/10.5194/essd-5-393-2013, 2013
G. Hugelius, C. Tarnocai, G. Broll, J. G. Canadell, P. Kuhry, and D. K. Swanson
Earth Syst. Sci. Data, 5, 3–13, https://doi.org/10.5194/essd-5-3-2013, https://doi.org/10.5194/essd-5-3-2013, 2013
Cited articles
Appelhans, T., Mwangomo, E., Otte, I., Detsch, F., Nauss, T., and Hemp, A.:
Eco-Meteorological Characteristics of the Southern Slopes of Kilimanjaro,
Tanzania, Int. J. Climatol., 36, 3245–3258, https://doi.org/10.1002/joc.4552,
2016. a, b
Beniston, M., Diaz, H. F., and Bradley, R. S.: Climatic Change at High
Elevation Sites: An Overview, Climatic Change, 36, 233–251,
https://doi.org/10.1007/978-94-015-8905-5_1, 1997. a
Bittner, L., Gil-Romera, G., Grady, D., Lamb, H. F., Lorenz, E., Weiner, M.,
Meyer, H., Bromm, T., Glaser, B., and Zech, M.: The Holocene
Lake-Evaporation History of the Afro-Alpine Lake Garba Guracha in the
Bale Mountains, Ethiopia, Based on δ18O Records of Sugar Biomarker and Diatoms, Quaternary Res., 1–14,
https://doi.org/10.1017/qua.2021.26, online first, 2021. a
Bojinski, S., Verstraete, M., Peterson, T. C., Richter, C., Simmons, A., and
Zemp, M.: The Concept of Essential Climate Variables in Support
of Climate Research, Applications, and Policy, B. Am.
Meteorol. Soc., 95, 1431–1443, https://doi.org/10.1175/BAMS-D-13-00047.1, 2014. a
Buytaert, W., Célleri, R., De Bièvre, B., Cisneros, F., Wyseure, G.,
Deckers, J., and Hofstede, R.: Human Impact on the Hydrology of the
Andean Páramos, Earth-Sci. Rev., 79, 53–72,
https://doi.org/10.1016/j.earscirev.2006.06.002, 2006. a
Buytaert, W., Cuesta-Camacho, F., and Tobón, C.: Potential Impacts of
Climate Change on the Environmental Services of Humid Tropical Alpine
Regions: Climate Change and Environmental Services, Glob. Ecol.
Biogeogr., 20, 19–33, https://doi.org/10.1111/j.1466-8238.2010.00585.x, 2011. a, b, c
Chignell, S. M., Laituri, M. J., Young, N. E., and Evangelista, P. H.:
Afroalpine Wetlands of the Bale Mountains, Ethiopia:
Distribution, Dynamics, and Conceptual Flow Model, Ann. Am.
Assoc. Geogr., 109, 791–811, https://doi.org/10.1080/24694452.2018.1500439, 2019. a
Collier, E., Sauter, T., Mölg, T., and Hardy, D.: The Influence of
Tropical Cyclones on Circulation, Moisture Transport, and Snow
Accumulation at Kilimanjaro During the 2006–2007 Season,
J. Geophys. Res.-Atmos., 124, 2019JD030682, https://doi.org/10.1029/2019JD030682, 2019. a
Colwell, R. K., Brehm, G., Cardelus, C. L., Gilman, A. C., and Longino, J. T.:
Global Warming, Elevational Range Shifts, and Lowland Biotic
Attrition in the Wet Tropics, Science, 322, 258–261,
https://doi.org/10.1126/science.1162547, 2008. a
Costa, K., Russell, J., Konecky, B., and Lamb, H.: Isotopic Reconstruction of
the African Humid Period and Congo Air Boundary Migration at Lake
Tana, Ethiopia, Quaternary Sci. Rev., 83, 58–67,
https://doi.org/10.1016/j.quascirev.2013.10.031, 2014. a
Diaz, H. F. and Bradley, R. S.: Temperature Variations During the Last
Century at High Elevation Sites, Clim. Chang., 36, 253–279,
https://doi.org/10.1007/978-94-015-8905-5_2, 1997. a, b
Frauenfelder, R., Isaksen, K., Lato, M. J., and Noetzli, J.: Ground thermal and geomechanical conditions in a permafrost-affected high-latitude rock avalanche site (Polvartinden, northern Norway), The Cryosphere, 12, 1531–1550, https://doi.org/10.5194/tc-12-1531-2018, 2018. a
Gebrechorkos, S. H., Hülsmann, S., and Bernhofer, C.: Long-Term Trends in
Rainfall and Temperature Using High-Resolution Climate Datasets in East
Africa, Sci. Rep., 9, 1–9, https://doi.org/10.1038/s41598-019-47933-8, 2019. a
Geotest: UTL-3 Temperature Datalogger,
https://www.geotest.ch/en/innovation/utl-temperature-datalogger, last
access: 22 February 2021. a
Gil-Romera, G., Adolf, C., Benito, B. M., Bittner, L., Johansson, M. U.,
Grady, D. A., Lamb, H. F., Lemma, B., Fekadu, M., Glaser, B., Mekonnen, B.,
Sevilla-Callejo, M., Zech, M., Zech, W., and Miehe, G.: Long-Term Fire
Resilience of the Ericaceous Belt, Bale Mountains, Ethiopia,
Biol. Lett., 15, 20190357, https://doi.org/10.1098/rsbl.2019.0357, 2019. a
Gottelli, D. and Sillero-Zubiri, C.: The Simien Jackal: Ecology and
Conservation. The Bale Mountains Research Project, Wildlife
Conservation International, New York, 1990. a
Gottelli, D., Sillero-Zubiri, C., Applebaum, G. D., Roy, M. S., Girman,
D. J., Garcia-Moreno, J., Ostrander, E. A., and Wayne, R. K.: Molecular
Genetics of the Most Endangered Canid: The Ethiopian Wolf Canis
Simensis, Mol. Ecol., 3, 301–312, https://doi.org/10.1111/j.1365-294X.1994.tb00070.x,
1994. a
Grab, S. W., Gatebe, C. K., and Kinyua, A. M.: Ground Thermal Profiles from
Mount Kenya, East Africa, Geogr. Ann. Ser. A, 86, 131–141,
https://doi.org/10.1111/j.0435-3676.2004.00219.x, 2004. a, b, c, d
Groos, A. R., Niederhauser, J., Lemma, B., Fekadu, M., Zech, W., Hänsel,
F., Wraase, L., Akçar, N., and Veit, H.: An hourly ground temperature
dataset for 16 high elevation sites (3493–4377 m a.s.l.) in the Bale
Mountains, Ethiopia (2017–2020) (v1.1.2), Zenodo [data set],
https://doi.org/10.5281/zenodo.6047457, 2022. a, b, c, d
Hendrickx, H., Jacob, M., Frankl, A., Guyassa, E., and Nyssen, J.: Quaternary
Glacial and Periglacial Processes in the Ethiopian Highlands in Relation
to the Current Afro-Alpine Vegetation, Z. Geomorphol., 59, 37–57,
https://doi.org/10.1127/0372-8854/2014/0128, 2014. a
Hillman, J. C.: Bale Mountains National Park : management plan, Ethiopian Wildlife Conservation Organisation, Ministry of Agriculture, Addis Ababa, Ethiopia, 250 pp., 1986. a
Hoelzle, M., Wegmann, M., and Krummenacher, B.: Miniature Temperature
Dataloggers for Mapping and Monitoring of Permafrost in High Mountain Areas:
First Experience from the Swiss Alps, Permafrost Periglac., 10,
113–124,
https://doi.org/10.1002/(SICI)1099-1530(199904/06)10:2<113::AID-PPP317>3.0.CO;2-A,
1999. a
Imhof, M., Pierrehumbert, G., Haeberli, W., and Kienholz, H.: Permafrost
Investigation in the Schilthorn Massif, Bernese Alps,
Switzerland, Permafrost Periglac., 11, 189–206,
https://doi.org/10.1002/1099-1530(200007/09)11:3<189::AID-PPP348>3.0.CO;2-N, 2000. a
Kaser, G.: A Review of the Modern Fluctuations of Tropical Glaciers, Global
Planet. Change, 22, 93–103, https://doi.org/10.1016/S0921-8181(99)00028-4, 1999. a
Kaser, G., Großhauser, M., and Marzeion, B.: Contribution Potential of
Glaciers to Water Availability in Different Climate Regimes, P. Natl.
Acad. Sci. USA, 107, 20223–20227, https://doi.org/10.1073/pnas.1008162107, 2010. a
Kraaijenbrink, P. D. A., Shea, J. M., Litt, M., Steiner, J. F., Treichler, D.,
Koch, I., and Immerzeel, W. W.: Mapping Surface Temperatures on a
Debris-Covered Glacier With an Unmanned Aerial Vehicle, Front.
Earth Sci., 6, 1–19, https://doi.org/10.3389/feart.2018.00064, 2018. a, b
Lemma, B., Mekonnen, B., Glaser, B., Zech, W., Nemomissa, S., Bekele, T., Bittner, L., and Zech, M.: Chemotaxonomic patterns of vegetation and soils along altitudinal transects of the Bale Mountains, Ethiopia, and implications for paleovegetation reconstructions – Part II: lignin-derived phenols and leaf-wax-derived n-alkanes, E&G Quaternary Sci. J., 68, 189–200, https://doi.org/10.5194/egqsj-68-189-2019, 2019. a, b
Lemma, B., Kebede Gurmessa, S., Nemomissa, S., Otte, I., Glaser, B., and Zech,
M.: Spatial and Temporal 2H and 18O Isotope Variation
of Contemporary Precipitation in the Bale Mountains, Ethiopia, Isot.
Environ. Health Stud., 56, 1–14, https://doi.org/10.1080/10256016.2020.1717487, 2020. a, b
Lepot, M., Aubin, J.-B., and Clemens, F.: Interpolation in Time Series:
An Introductive Overview of Existing Methods, Their Performance
Criteria and Uncertainty Assessment, Water, 9, 796,
https://doi.org/10.3390/w9100796, 2017. a
Levin, N. E., Zipser, E. J., and Cerling, T. E.: Isotopic Composition of Waters
from Ethiopia and Kenya: Insights into Moisture Sources for
Eastern Africa, J. Geophys. Res., 114, 1–13, https://doi.org/10.1029/2009JD012166,
2009. a
Marino, J., Sillero-Zubiri, C., and Macdonald, D.: Trends, Dynamics and
Resilience of an Ethiopian Wolf Population, Anim. Conserv., 9, 49–58,
https://doi.org/10.1111/j.1469-1795.2005.00011.x, 2006. a
Mekonnen, B., Zech, W., Glaser, B., Lemma, B., Bromm, T., Nemomissa, S., Bekele, T., and Zech, M.: Chemotaxonomic patterns of vegetation and soils along altitudinal transects of the Bale Mountains, Ethiopia, and implications for paleovegetation reconstructions – Part 1: stable isotopes and sugar biomarkers, E&G Quaternary Sci. J., 68, 177–188, https://doi.org/10.5194/egqsj-68-177-2019, 2019. a
Mohr, P.: Ethiopian Flood Basalt Province, Nature, 303, 577–584,
https://doi.org/10.1038/303577a0, 1983. a
Mölg, T., Hardy, D. R., Collier, E., Kropač, E., Schmid, C., Cullen, N. J., Kaser, G., Prinz, R., and Winkler, M.: Mesoscale atmospheric circulation controls of local meteorological elevation gradients on Kersten Glacier near Kilimanjaro summit, Earth Syst. Dynam., 11, 653–672, https://doi.org/10.5194/esd-11-653-2020, 2020. a
Mosquera, G. M., Lazo, P. X., Célleri, R., Wilcox, B. P., and Crespo, P.:
Runoff from Tropical Alpine Grasslands Increases with Areal Extent of
Wetlands, Catena, 125, 120–128, https://doi.org/10.1016/j.catena.2014.10.010, 2015. a
Nicholson, L. I., Prinz, R., Mölg, T., and Kaser, G.: Micrometeorological conditions and surface mass and energy fluxes on Lewis Glacier, Mt Kenya, in relation to other tropical glaciers, The Cryosphere, 7, 1205–1225, https://doi.org/10.5194/tc-7-1205-2013, 2013. a
Osmaston, H. A., Mitchell, W. A., and Osmaston, J. A. N.: Quaternary Glaciation
of the Bale Mountains, Ethiopia, J. Quaternary Sci., 20, 593–606,
https://doi.org/10.1002/jqs.931, 2005. a, b, c
Ossendorf, G., Groos, A. R., Bromm, T., Tekelemariam, M. G., Glaser, B., Lesur,
J., Schmidt, J., Akçar, N., Bekele, T., Beldados, A., Demissew, S.,
Kahsay, T. H., Nash, B. P., Nauss, T., Negash, A., Nemomissa, S., Veit, H.,
Vogelsang, R., Woldu, Z., Zech, W., Opgenoorth, L., and Miehe, G.: Middle
Stone Age Foragers Resided in High Elevations of the Glaciated Bale
Mountains, Ethiopia, Science, 365, 583–587,
https://doi.org/10.1126/science.aaw8942, 2019. a
Pepin, N. C. and Lundquist, J. D.: Temperature Trends at High Elevations:
Patterns across the Globe, Geophys. Res. Lett., 35, L14701,
https://doi.org/10.1029/2008GL034026, 2008. a
Pepin, N. C. and Seidel, D. J.: A Global Comparison of Surface and Free-Air
Temperatures at High Elevations, J. Geophys. Res., 110, D03104,
https://doi.org/10.1029/2004JD005047, 2005. a, b
Pepin, N. C., Bradley, R. S., Diaz, H. F., Baraer, M., Caceres, E. B.,
Forsythe, N., Fowler, H., Greenwood, G., Hashmi, M. Z., Liu, X. D., Miller,
J. R., Ning, L., Ohmura, A., Palazzi, E., Rangwala, I., Schöner, W.,
Severskiy, I., Shahgedanova, M., Wang, M. B., Williamson, S. N., and Yang,
D. Q.: Elevation-Dependent Warming in Mountain Regions of the World, Nat.
Clim. Change, 5, 424–430, https://doi.org/10.1038/nclimate2563, 2015. a, b, c
Pepin, N. C., Maeda, E. E., and Williams, R.: Use of Remotely Sensed Land
Surface Temperature as a Proxy for Air Temperatures at High Elevations:
Findings from a 5000 m Elevational Transect across Kilimanjaro:
MODIS LST versus Tair at high
elevations, J. Geophys. Res.-Atmos., 121, 9998–10015,
https://doi.org/10.1002/2016JD025497, 2016. a, b
Peters, M. K., Hemp, A., Appelhans, T., Becker, J. N., Behler, C., Classen, A.,
Detsch, F., Ensslin, A., Ferger, S. W., Frederiksen, S. B., Gebert, F.,
Gerschlauer, F., Gütlein, A., Helbig-Bonitz, M., Hemp, C., Kindeketa,
W. J., Kühnel, A., Mayr, A. V., Mwangomo, E., Ngereza, C., Njovu, H. K.,
Otte, I., Pabst, H., Renner, M., Röder, J., Rutten, G.,
Schellenberger Costa, D., Sierra-Cornejo, N., Vollstädt, M. G. R.,
Dulle, H. I., Eardley, C. D., Howell, K. M., Keller, A., Peters, R. S.,
Ssymank, A., Kakengi, V., Zhang, J., Bogner, C., Böhning-Gaese, K.,
Brandl, R., Hertel, D., Huwe, B., Kiese, R., Kleyer, M., Kuzyakov, Y., Nauss,
T., Schleuning, M., Tschapka, M., Fischer, M., and Steffan-Dewenter, I.:
Climate–Land-Use Interactions Shape Tropical Mountain Biodiversity
and Ecosystem Functions, Nature, 568, 88–92,
https://doi.org/10.1038/s41586-019-1048-z, 2019. a, b, c
Qin, J., Yang, K., Liang, S., and Guo, X.: The Altitudinal Dependence of Recent
Rapid Warming over the Tibetan Plateau, Climatic Change, 97, 321–327,
https://doi.org/10.1007/s10584-009-9733-9, 2009.
a
Rahbek, C., Borregaard, M. K., Colwell, R. K., Dalsgaard, B., Holt, B. G.,
Morueta-Holme, N., Nogues-Bravo, D., Whittaker, R. J., and Fjeldså,
J.: Humboldt's Enigma: What Causes Global Patterns of Mountain
Biodiversity?, Science, 365, 1108–1113, https://doi.org/10.1126/science.aax0149, 2019. a, b
Rangwala, I. and Miller, J. R.: Climate Change in Mountains: A Review of
Elevation-Dependent Warming and Its Possible Causes, Climatic Change, 114,
527–547, https://doi.org/10.1007/s10584-012-0419-3, 2012. a, b
Rist, A., Roth, L., and Veit, H.: Elevational Ground/Air Thermal Gradients in
the Swiss Inner Alpine Valais, Arct. Antarct. Alp. Res., 52,
341–360, https://doi.org/10.1080/15230430.2020.1742022, 2020. a
Schrott, L., Otto, J.-C., and Keller, F.: Modelling Alpine Permafrost
Distribution in the Hohe Tauern Region, Austria, Austrian J. Earth
Sci., 105, 169–183, 2012. a
Seleshi, Y. and Zanke, U.: Recent Changes in Rainfall and Rainy Days in
Ethiopia, Int. J. Climatol., 24, 973–983, https://doi.org/10.1002/joc.1052, 2004. a
Tempmate: Temperature and humidity miniature data logger,
https://www.tempmate.com/temperature-logger/tempmate-b-series/, last
access: 22 February 2021. a
Tierney, J. E., Russell, J. M., Sinninghe Damsté, J. S., Huang, Y., and
Verschuren, D.: Late Quaternary Behavior of the East African Monsoon
and the Importance of the Congo Air Boundary, Quaternary Sci. Rev., 30,
798–807, https://doi.org/10.1016/j.quascirev.2011.01.017, 2011. a
Veettil, B. K. and Kamp, U.: Global Disappearance of Tropical Mountain
Glaciers: Observations, Causes, and Challenges, Geosciences, 9,
1–25, https://doi.org/10.3390/geosciences9050196, 2019. a
Vieira, G., Mora, C., and Faleh, A.: New observations indicate the possible presence of permafrost in North Africa (Djebel Toubkal, High Atlas, Morocco), The Cryosphere, 11, 1691–1705, https://doi.org/10.5194/tc-11-1691-2017, 2017. a, b, c
Vlasatá, T., Šklíba, J., Lövy, M., Meheretu, Y.,
Sillero-Zubiri, C., and Šumbera, R.: Daily Activity Patterns in the
Giant Root Rat (Tachyoryctes Macrocephalus), a Fossorial Rodent from the
Afro-Alpine Zone of the Bale Mountains, Ethiopia, J. Zool., 302,
157–163, https://doi.org/10.1111/jzo.12441, 2017. a
Wöllauer, S., Zeuss, D., Hänsel, F., and Nauss, T.: TubeDB: An
on-Demand Processing Database System for Climate Station Data, Comput.
Geosci., 146, 104641, https://doi.org/10.1016/j.cageo.2020.104641, 2020. a, b
Short summary
Continuous observations and measurements from high elevations are necessary to monitor recent climate and environmental changes in the tropical mountains of eastern Africa, but meteorological and ground temperature data from above 3000 m are very rare. Here we present a comprehensive ground temperature monitoring network that has been established between 3493 and 4377 m in the Bale Mountains (Ethiopian Highlands) to monitor and study the afro-alpine climate and ecosystem in this region.
Continuous observations and measurements from high elevations are necessary to monitor recent...
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