Klinge, Michael

[["dc.bibliographiccitation.firstpage","59"],["dc.bibliographiccitation.journal","Geomorphology"],["dc.bibliographiccitation.lastpage","71"],["dc.bibliographiccitation.volume","292"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.contributor.author","Schulte, Philipp"],["dc.contributor.author","Hülle, Daniela"],["dc.contributor.author","Nottebaum, Veit"],["dc.date.accessioned","2020-12-10T14:24:19Z"],["dc.date.available","2020-12-10T14:24:19Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1016/j.geomorph.2017.04.027"],["dc.identifier.issn","0169-555X"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/72217"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Implications of (reworked) aeolian sediments and paleosols for Holocene environmental change in Western Mongolia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","100628"],["dc.bibliographiccitation.journal","Aeolian Research"],["dc.bibliographiccitation.volume","47"],["dc.contributor.author","Bertran, Pascal"],["dc.contributor.author","Andrieux, Eric"],["dc.contributor.author","Bateman, Mark D."],["dc.contributor.author","Fuchs, Markus"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Marembert, Fabrice"],["dc.date.accessioned","2021-04-14T08:30:21Z"],["dc.date.available","2021-04-14T08:30:21Z"],["dc.date.issued","2020"],["dc.identifier.doi","10.1016/j.aeolia.2020.100628"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/83200"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-399"],["dc.relation.issn","1875-9637"],["dc.title","Mapping and chronology of coversands and dunes from the Aquitaine basin, southwest France"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","117"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","132"],["dc.bibliographiccitation.volume","68"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Rees-Jones, J."],["dc.contributor.author","Rhodes, E. J."],["dc.date.accessioned","2018-11-07T11:15:27Z"],["dc.date.available","2018-11-07T11:15:27Z"],["dc.date.issued","2000"],["dc.description.abstract","The geomorphology and the cover sediments in the central and south-eastern part of the Tibetan Plateau provide information about climatic change. Luminescence dating of aeolian and colluvial silts on top of different moraine sequences provides the first indications for the timing of these sediments during the Late Quaternary and Holocene. Although there is a widespread cover of aeolian mantles in Tibet, only a few payers have focussed on them up to now. Samples from silt layers on top of Pleistocene moraines or solifluction debris from central and southern Tibet at elevations above 4000 m asl provide early Holocene ages in most sections. The aeolian silt on top of the \"Bomi-moraine\" in southeastern Tibet situated at an elevation of about 3000 m asl, provides an age of 25 ka. According to geomorphological investigations the Bomi moraine dates from the last ice age, which can be confirmed by the luminescence data. Moreover, one sample from a silt layer in-between gravel layers (Xainxa) is also Pleistocene in age according to its sedimentary and geomorphological situation. In the Tibetan Plateau Pleistocene loess mainly occurs below 4000 m asl. the Holocene material, a more sandy silt, lying above 4000 m asl. However, aeolian material capping the moraines provides only minimum ages for the terminal moraines: the time interval between glacier retreat and the accumulation of aeolian sediments may be several thousand years. The most important fact is the trapping of dust. In general, lakes and a denser vegetation cover are or were the main traps for the typical loess found in the mountain areas of the Tibetan Plateau. (C) 2000 Elsevier Science Ltd and INQUA. All rights reserved."],["dc.identifier.doi","10.1016/S1040-6182(00)00038-0"],["dc.identifier.isi","000089483800012"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/54366"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","1040-6182"],["dc.title","Late Quaternary aeolian sedimentation in central and south-eastern Tibet"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","780"],["dc.bibliographiccitation.journal","Forest Ecology and Management"],["dc.bibliographiccitation.lastpage","788"],["dc.bibliographiccitation.volume","433"],["dc.contributor.author","Dulamsuren, Choimaa"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Bat-Enerel, Banzragch"],["dc.contributor.author","Ariunbaatar, Tumurbaatar"],["dc.contributor.author","Tuya, Daramragchaa"],["dc.date.accessioned","2019-07-17T13:23:04Z"],["dc.date.available","2019-07-17T13:23:04Z"],["dc.date.issued","2019"],["dc.description.abstract","The hypothesis was tested that the size and the degree of isolation of Larix sibirica forests in the forest-steppe ecotone of Mongolia affects aboveground and belowground carbon pool densities. The research question was based on the fact that both microclimate and the drought sensitivity of stemwood production were earlier shown to differ with stand size and isolation in this ecotone. Contrary to our hypothesis, we did not find significant differences in the organic carbon stock densities of the tree biomass and the mineral soil. The depth, carbon content and carbon stock density of the organic layer increased with stand size, but was not a major determinant of total ecosystem carbon stock density. Nevertheless, the increasing depth and the increasing humus content of the organic layer with stand size could be significant by improving moisture availability and, thus, promoting forest regeneration. Furthermore, reduced organic layer thickness and humus content and thus water storage capacity could be one out of several causes of the previously observed higher drought vulnerability of stemwood formation in small forest stands of the Mongolian forest-steppe. A mean carbon stock density of 237 Mg C ha⁻¹ for total ecosystem organic carbon stock density matches with earlier estimates for Mongolia's boreal forest corroborating the view that the ecosystem carbon pool density at the southern edge of the boreal forest is lower compared to forests at higher latitudes with even colder climate and deeper and more widespread permafrost."],["dc.identifier.doi","10.1016/j.foreco.2018.10.054"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61718"],["dc.language.iso","en"],["dc.relation.issn","0378-1127"],["dc.title","Effects of forest fragmentation on organic carbon pool densities in the Mongolian forest-steppe"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","2893"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Biogeosciences"],["dc.bibliographiccitation.lastpage","2905"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Bohner, J."],["dc.contributor.author","Erasmi, Stefan"],["dc.date.accessioned","2018-11-07T10:03:10Z"],["dc.date.accessioned","2020-05-11T13:23:57Z"],["dc.date.available","2018-11-07T10:03:10Z"],["dc.date.available","2020-05-11T13:23:57Z"],["dc.date.issued","2015"],["dc.description.abstract","Satellite images and digital elevation models provide an excellent database to analyze forest distribution patterns and forest limits in the mountain regions of semiarid central Asia on the regional scale. For the investigation area in the northern Tien Shan, a strong relationship between forest distribution and climate conditions could be found. Additionally areas of potential human impact on forested areas are identified at lower elevations near the edge of the mountains based on an analysis of the differences in climatic preconditions and the present occurrence of forest stands. The distribution of spruce (Picea schrenkiana) forests is hydrologically limited by a minimum annual precipitation of 250 mm and thermally by a minimum monthly mean temperature of 5 degrees C during the growing season. While the actual lower forest limit increases from 1600 m a.s.l. (above sea level) in the northwest to 2600 m a.s.l. in the southeast, the upper forest limit rises in the same direction from 1800 m a.s.l. to 2900 m a.s.l.. In accordance with the main wind directions, the steepest gradient of both forest lines and the greatest local vertical extent of the forest belt of 500 to 600 m to a maximum of 900 m occur at the northern and western mountain fronts. The forests in the investigation area are strongly restricted to north-facing slopes, which is a common feature in semiarid central Asia. Based on the presumption that variations in local climate conditions are a function of topography, the potential forest extent was analyzed with regard to the parameters slope, aspect, solar radiation input and elevation. All four parameters showed a strong relationship to forest distribution, yielding a total potential forest area that is 3.5 times larger than the present forest remains of 502 km(2)."],["dc.identifier.doi","10.5194/bg-12-2893-2015"],["dc.identifier.isi","000356179300006"],["dc.identifier.scopus","2-s2.0-84930216355"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/65048"],["dc.identifier.url","http://www.scopus.com/inward/record.url?eid=2-s2.0-84930216355&partnerID=MN8TOARS"],["dc.language.iso","en"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.eissn","1726-4170"],["dc.relation.issn","1726-4189"],["dc.title","Modeling forest lines and forest distribution patterns with remote-sensing data in a mountainous region of semiarid central Asia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","75"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Zeitschrift für Geomorphologie"],["dc.bibliographiccitation.lastpage","102"],["dc.bibliographiccitation.volume","44"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.contributor.author","Klinge, Michael"],["dc.date.accessioned","2018-11-07T09:48:16Z"],["dc.date.available","2018-11-07T09:48:16Z"],["dc.date.issued","2000"],["dc.description.abstract","In the continental areas of Central Asia periglacial features and processes are mainly determined through existence of soil humidity during the freeze-thaw cycles. Hourly measurements of the soil temperatures of different depths at distinct geoecological sites were carried out in two measuring cycles 1995/96 and 1997/98 lasting almost 11 month. The detailed studies focussed on mountain areas of the northern Mongolian Altai (Turgen-Kharkhiraa mountains) in elevations between 1775 and 2760 m a. s.l. The main difference in the intensity of periglacial processes in the basins and mountains areas, respectively, can be seen in the freeze-thaw cycles in spring time, mainly in April. In this time the precipitation in the mountains is still snow fall and moisture can infiltrate into the soils. Due to higher temperature the precipitation (mainly min) in the basins evaporate and rapid drying out of the soils occurs. The main controlling factor for the cryogenic processes in the mountains (especially of solifluction) therefore is the amount of precipitation during spring time. The freeze-thaw cycles during the relatively dry autumn season are subordinated factor for the geomorphological activity. At sites with low radiation, as caused e. g. through shading effects in relief, the freeze-thaw cycles displace towards the summer with more precipitation. Therefore, periglacial processes on low-radiation sites are laced to the strength of the summer precipitation. On the other hand, the frequent freeze-thaw cycles at sites with high radiation drop towards the dry winter season and therefore, the periglacial activity is low at such sites. Accumulation of snow (e. g, in nivation hollows) and/or the occurrence of frozen ground could guarantees sufficient soil humidity apart from the distribution of precipitation during the highest freeze-thaw cycles in the spring and autumn seasons and determines cryogenic processes and periglacial forms (e.g.earth hummocks, patterned grounds). This local influence can be reinforced by effects of radiation, In the Larix forests at northern slopes a cooler local climate with reduced transpiration in the summer allows the preservation of frozen ground and/or permafrost."],["dc.identifier.isi","000087341400004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/35269"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Gebruder Borntraeger"],["dc.relation.issn","0372-8854"],["dc.title","Soil temperature measurements from the Mongolian Altai as indicators for periglacial geomorphodynamics in continental mountain areas"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.journal","Earth Surface Processes and Landforms"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Schneider, Florian"],["dc.contributor.author","Dulamsuren, Choimaa"],["dc.contributor.author","Arndt, Kim"],["dc.contributor.author","Bayarsaikhan, Uudus"],["dc.contributor.author","Sauer, Daniela"],["dc.date.accessioned","2021-06-01T09:41:48Z"],["dc.date.available","2021-06-01T09:41:48Z"],["dc.date.issued","2021"],["dc.identifier.doi","10.1002/esp.5116"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/85043"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-425"],["dc.relation.eissn","1096-9837"],["dc.relation.issn","0197-9337"],["dc.title","Interrelations between relief, vegetation, disturbances, and permafrost in the forest‐steppe of central Mongolia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1205"],["dc.bibliographiccitation.issue","9"],["dc.bibliographiccitation.journal","ZEITSCHRIFT FUR PHYSIKALISCHE CHEMIE-INTERNATIONAL JOURNAL OF RESEARCH IN PHYSICAL CHEMISTRY & CHEMICAL PHYSICS"],["dc.bibliographiccitation.lastpage","1222"],["dc.bibliographiccitation.volume","219"],["dc.contributor.author","Buback, M."],["dc.contributor.author","Kling, M."],["dc.contributor.author","Schmatz, S."],["dc.date.accessioned","2018-11-07T08:50:10Z"],["dc.date.available","2018-11-07T08:50:10Z"],["dc.date.issued","2005"],["dc.description.abstract","Rate coefficients of beta-scission reactions in tertiary alkoxy radicals, R(CH3)(2)CO (R = methyl, ethyl, tert-butyl and neo-pentyl) have been estimated via density functional theory (DFT) calculations in conjunction with statistical unimolecular rate theory. For tert-butoxy, results obtained by employing different basis sets are compared with experimental values, indicating that UB3LYP/6-31G(d,p) excellently predicts kinetic data. Rate coefficients for inter- and intramolecular hydrogen abstraction are also reported. Depending on R, the P-scission rate may vary by orders of magnitude. The predicted temperature dependence of the alcohol-to-ketone product ratios for alkoxy radical decomposition in a hydrocarbon environment is in remarkably close agreement with the corresponding ratios measured on the product mixtures from decomposition of tert-butyl and tert-amyl peroxyacetates in solution of n-heptane."],["dc.identifier.doi","10.1524/zpch.2005.219.9.1205"],["dc.identifier.isi","000232490800002"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/21635"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Oldenbourg Verlag"],["dc.relation.issn","0942-9352"],["dc.title","Decomposition of tertiary alkoxy radicals"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Psychosomatic Medicine"],["dc.bibliographiccitation.volume","63"],["dc.contributor.author","Herrmann-Lingen, Christoph"],["dc.contributor.author","Binder, L."],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Sander, Josemir W."],["dc.contributor.author","Schenker, W."],["dc.contributor.author","Pieske, Burkert M."],["dc.date.accessioned","2018-11-07T09:38:58Z"],["dc.date.available","2018-11-07T09:38:58Z"],["dc.date.issued","2001"],["dc.format.extent","182"],["dc.identifier.isi","000166843200316"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/33178"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Lippincott Williams & Wilkins"],["dc.publisher.place","Philadelphia"],["dc.relation.issn","0033-3174"],["dc.title","Neuroendocrine activation is unrelated to depressed mood and vital exhaustion in patients with chronic heart failure"],["dc.type","conference_abstract"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","33"],["dc.bibliographiccitation.journal","Quaternary International"],["dc.bibliographiccitation.lastpage","44"],["dc.bibliographiccitation.volume","372"],["dc.contributor.author","Klinge, Michael"],["dc.contributor.author","Lehmkuhl, Frank"],["dc.date.accessioned","2018-11-07T09:55:45Z"],["dc.date.available","2018-11-07T09:55:45Z"],["dc.date.issued","2015"],["dc.description.abstract","On the southern Tibetan Plateau (TP) a sediment cover of aeolian sand and silt is widely distributed beyond the basins in an elevation belt above 4000 m asl. In this geomorphological environment a continuous aeolian sedimentation occurred during the Holocene and erosion processes kept subordinate until late Holocene. A dark humic paleosol, which is dated to between 4100 and 2000 years cal BP, divides the aeolian sediment cover into two stratigraphic units. The lower unit started with the beginning of the aeolian sedimentation since late Glacial and early Holocene and extended until mid-Holocene when the paleosol developed. The sediments show the bright color of fresh loess-like material and no paleosol representing the early to mid-Holocene climate optimum is detected. The upper sediment unit started after the end of paleosol development and lasted until the late Holocene with an increased deposition of re-transported loess. The enhanced aeolian sediment mobilization during late Holocene is provoked by drier and cooler climatic conditions reducing the vegetation density. In addition, human impact on the vegetation by overgrazing of livestock and forest clearing enforced soil erosion processes and thus the supply of fine material. The modern soil and vegetation cover on top of this sediment unit are related to the modern climatic conditions. In the semi-arid region surrounding the lakes Nam Co and Siling Co alpine steppe vegetation and phaeozem soils occur. In the southern part which is more humid, alpine meadow vegetation with cambisols appears. All the paleosols are of cambisol type and therefore represent a more humid period from the upper boundary of mid-Holocene until the beginning of late Holocene, because of higher availability of effective moisture for the growth of dense vegetation cover and appropriate paleosol formation. For this period of paleosol development a general trend from north to south is obvious: from 5.5 to 3.8 ka BP in the northeastern TP to between 4.1 and 2 ka BP in the southern TP. This coincides with the observed retreat of monsoonal precipitation on the TP during that time. In contrast to the arid and semi-arid environment of the TP the amount of precipitation is not the primary limiting factor for vegetation density and soil development, but temperature and solar radiation have a great influence on local evapotranspiration and effective moisture. (C) 2014 Elsevier Ltd and INQUA. All rights reserved."],["dc.identifier.doi","10.1016/j.quaint.2014.06.068"],["dc.identifier.isi","000355674100005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/36819"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Pergamon-elsevier Science Ltd"],["dc.relation.issn","1873-4553"],["dc.relation.issn","1040-6182"],["dc.title","Holocene aeolian mantles and inter-bedded paleosols on the southern Tibetan Plateau"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]