Gerold, Gerhard

[["dc.bibliographiccitation.artnumber","e0182893"],["dc.bibliographiccitation.issue","8"],["dc.bibliographiccitation.journal","PloS one"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Gómez-Díaz, Jorge Antonio"],["dc.contributor.author","Krömer, Thorsten"],["dc.contributor.author","Kreft, Holger"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Carvajal-Hernández, César Isidro"],["dc.contributor.author","Heitkamp, Felix"],["dc.contributor.editor","Zang, RunGuo"],["dc.date.accessioned","2018-03-13T14:13:12Z"],["dc.date.available","2018-03-13T14:13:12Z"],["dc.date.issued","2017"],["dc.description.abstract","Terrestrial herbs are important elements of tropical forests; however, there is a lack of research on their diversity patterns and how they respond to different intensities of forest-use. The aim of this study was to analyze the diversity of herbaceous angiosperms along gradients of elevation (50 m to 3500 m) and forest-use intensity on the eastern slopes of the Cofre de Perote, Veracruz, Mexico. We recorded the occurrence of all herbaceous angiosperm species within 120 plots of 20 m x 20 m each. The plots were located at eight study locations separated by ~500 m in elevation and within three different habitats that differ in forest-use intensity: old-growth, degraded, and secondary forest. We analyzed species richness and floristic composition of herb communities among different elevations and habitats. Of the 264 plant species recorded, 31 are endemic to Mexico. Both α- and γ-diversity display a hump-shaped relation to elevation peaking at 2500 m and 3000 m, respectively. The relative contribution of between-habitat β-diversity to γ-diversity also showed a unimodal hump whereas within-habitat β-diversity declined with elevation. Forest-use intensity did not affect α-diversity, but β-diversity was high between old-growth and secondary forests. Overall, γ-diversity peaked at 2500 m (72 species), driven mainly by high within- and among-habitat β-diversity. We infer that this belt is highly sensitive to anthropogenic disturbance and forest-use intensification. At 3100 m, high γ-diversity (50 species) was driven by high α- and within-habitat β-diversity. There, losing a specific forest area might be compensated if similar assemblages occur in nearby areas. The high β-diversity and endemism suggest that mixes of different habitats are needed to sustain high γ-richness of terrestrial herbs along this elevational gradient."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2017"],["dc.identifier.doi","10.1371/journal.pone.0182893"],["dc.identifier.pmid","28792536"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14598"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/13012"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.relation.eissn","1932-6203"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Diversity and composition of herbaceous angiosperms along gradients of elevation and forest-use intensity"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","e47192"],["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","PloS one"],["dc.bibliographiccitation.lastpage","7"],["dc.bibliographiccitation.volume","7"],["dc.contributor.author","Kessler, Michael"],["dc.contributor.author","Hertel, Dietrich"],["dc.contributor.author","Jungkunst, Hermann F."],["dc.contributor.author","Kluge, Jürgen"],["dc.contributor.author","Abrahamczyk, Stefan"],["dc.contributor.author","Bos, Merijn Marinus"],["dc.contributor.author","Buchori, Damayanti"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Gradstein, S. Robbert"],["dc.contributor.author","Köhler, Stefan"],["dc.contributor.author","Leuschner, Christoph"],["dc.contributor.author","Moser, Gerald"],["dc.contributor.author","Pitopang, Ramadhanil"],["dc.contributor.author","Saleh, Shahabuddin"],["dc.contributor.author","Schulze, Christian Hansjoachim"],["dc.contributor.author","Sporn, Simone Goda"],["dc.contributor.author","Steffan-Dewenter, Ingolf"],["dc.contributor.author","Tjitrosoedirdjo, Sri Sudarmiyati"],["dc.contributor.author","Tscharntke, Teja"],["dc.contributor.editor","Bond-Lamberty, Ben"],["dc.date.accessioned","2018-07-05T16:08:40Z"],["dc.date.available","2018-07-05T16:08:40Z"],["dc.date.issued","2012"],["dc.description.abstract","Managing ecosystems for carbon storage may also benefit biodiversity conservation, but such a potential ‘win-win’ scenario has not yet been assessed for tropical agroforestry landscapes. We measured above- and below-ground carbon stocks as well as the species richness of four groups of plants and eight of animals on 14 representative plots in Sulawesi, Indonesia, ranging from natural rainforest to cacao agroforests that have replaced former natural forest. The conversion of natural forests with carbon stocks of 227–362 Mg C ha−1 to agroforests with 82–211 Mg C ha−1 showed no relationships to overall biodiversity but led to a significant loss of forest-related species richness. We conclude that the conservation of the forest-related biodiversity, and to a lesser degree of carbon stocks, mainly depends on the preservation of natural forest habitats. In the three most carbon-rich agroforestry systems, carbon stocks were about 60% of those of natural forest, suggesting that 1.6 ha of optimally managed agroforest can contribute to the conservation of carbon stocks as much as 1 ha of natural forest. However, agroforestry systems had comparatively low biodiversity, and we found no evidence for a tight link between carbon storage and biodiversity. Yet, potential win-win agroforestry management solutions include combining high shade-tree quality which favours biodiversity with cacao-yield adapted shade levels."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2012"],["dc.identifier.doi","10.1371/journal.pone.0047192"],["dc.identifier.gro","3150069"],["dc.identifier.pmid","23077569"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/8161"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/15169"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","final"],["dc.relation.issn","1932-6203"],["dc.rights","CC BY 2.5"],["dc.rights.uri","https://creativecommons.org/licenses/by/2.5"],["dc.title","Can Joint Carbon and Biodiversity Management in Tropical Agroforestry Landscapes Be Optimized?"],["dc.type","journal_article"],["dc.type.internalPublication","unknown"],["dc.type.peerReviewed","no"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","559"],["dc.bibliographiccitation.journal","Journal of Tropical Ecology"],["dc.bibliographiccitation.lastpage","562"],["dc.bibliographiccitation.volume","24"],["dc.contributor.author","Garrido-Perez, Edgardo I."],["dc.contributor.author","Manuel Dupuy, Juan"],["dc.contributor.author","Duran-Garcia, Rafael"],["dc.contributor.author","Ucan-May, Mario"],["dc.contributor.author","Schnitzer, Stefan A."],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T11:11:40Z"],["dc.date.available","2018-11-07T11:11:40Z"],["dc.date.issued","2008"],["dc.identifier.doi","10.1017/S0266467408005221"],["dc.identifier.isi","000259950800011"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/9068"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/53487"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Cambridge Univ Press"],["dc.relation.issn","0266-4674"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Effects of lianas and Hurricane Wilma on tree damage in the Yucatan Peninsula, Mexico"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","393"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Plant and Soil"],["dc.bibliographiccitation.lastpage","403"],["dc.bibliographiccitation.volume","342"],["dc.contributor.author","le Mellec, Anne"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Michalzik, Beate"],["dc.date.accessioned","2018-11-07T08:56:47Z"],["dc.date.available","2018-11-07T08:56:47Z"],["dc.date.issued","2011"],["dc.description.abstract","Apart from the forest floor, the canopy of forested ecosystems functions as the second most important source for dissolved and particulate fractions of organic and inorganic C and N compounds. However, under mass outbreak situations of insect herbivores this flux path of organic matter is considerably intensified clearly exceeding C and N fluxes from the forest floor. In this paper we report on herbivore-altered C and N fluxes from the canopy to the forest floor and effects on forest floor nutrient fluxes during severe defoliating herbivory of the winter moth (Operophtera brumata) and the mottled umber moth (Eranis defoliaria) in an oak forest in Germany. Over the course of 6.5 months we followed the C and N fluxes with bulk deposition, throughfall solution, insect frass deposits (green-fall together with insect faeces) and with forest floor solution in an 117-yr-old oak (Quercus petraea) forest. Compared to the control, herbivore defoliation significantly enhanced throughfall inputs of total and dissolved organic carbon and nitrogen by a factor of 3 and 2.5 (for TOC and DOC), and by 1.4 and 1.3 times (for TNb and DNb), respectively. Frass plus green-fall C and N fluxes peaked in May with 592 kg C ha(-1) and 33.5 kg N ha(-1) representing 79.6% (for C) and 78.3% (for N) of the total C and N input over 2.5 months. The quantitative and qualitative C and N input via faeces and litter deposition significantly differ between the insect affected and non-affected site. However, the C and N fluxes with throughfall did not significantly correlate with forest floor leachates. In this context, forest floor fluxes of TOC, DOC and NO3-N were significantly lower at the infested site compared to the control, whereas fluxes of NH4-N together with DON were significantly higher. The study demonstrates the importance of linking the population and associated frass dynamics of herbivorous insects with the cycling of nutrients and organic matter in forest ecosystems, highlighting the remarkable alterations in the timing, amounts and nature of organic matter dynamics on the ecosystem level. Consequently, the ecology of phytophagous insects allows partly to explain temporal-spatial alterations in nutrient cycling and thus ecosystem functioning."],["dc.description.sponsorship","German Research Foundation (DFG) [MI 927/1-3]"],["dc.identifier.doi","10.1007/s11104-010-0704-8"],["dc.identifier.isi","000289562000031"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/6662"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23233"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","1573-5036"],["dc.relation.issn","0032-079X"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Insect herbivory, organic matter deposition and effects on belowground organic matter fluxes in a central European oak forest"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","e0179414"],["dc.bibliographiccitation.issue","6"],["dc.bibliographiccitation.journal","PLoS ONE"],["dc.bibliographiccitation.volume","12"],["dc.contributor.author","Nobrega, Rodolfo L. B."],["dc.contributor.author","Guzha, Alphonce C."],["dc.contributor.author","Torres, Gilmar N."],["dc.contributor.author","Kovacs, Kristof"],["dc.contributor.author","Lamparter, Gabriele"],["dc.contributor.author","Amorim, Ricardo S. S."],["dc.contributor.author","Couto, Eduardo"],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T10:22:43Z"],["dc.date.available","2018-11-07T10:22:43Z"],["dc.date.issued","2017"],["dc.description.abstract","Understanding the impacts of land-use change on landscape-hydrological dynamics is one of the main challenges in the Northern Brazilian Cerrado biome, where the Amazon agricultural frontier is located. Motivated by the gap in literature assessing these impacts, we characterized the soil hydro-physical properties and quantified surface water fluxes from catchments under contrasting land-use in this region. We used data from field measurements in two headwater micro-catchments with similar physical characteristics and different land use, i.e. cerrado sensu stricto vegetation and pasture for extensive cattle ranching. We determined hydraulic and physical properties of the soils, applied ground-based remote sensing techniques to estimate evapotranspiration, and monitored streamflow from October 2012 to September 2014. Our results show significant differences in soil hydro-physical properties between the catchments, with greater bulk density and smaller total porosity in the pasture catchment. We found that evapotranspiration is smaller in the pasture ( 639 +/- 31% mm yr(-1)) than in the cerrado catchment ( 1,004 +/- 24% mm yr(-1)), and that streamflow from the pasture catchment is greater with runoff coefficients of 0.40 for the pasture and 0.27 for the cerrado catchment. Overall, our results confirm that conversion of cerrado vegetation to pasture causes soil hydro-physical properties deterioration, reduction in evapotranspiration reduction, and increased streamflow."],["dc.description.sponsorship","Open-Access-Publikationsfonds 2017"],["dc.identifier.doi","10.1371/journal.pone.0179414"],["dc.identifier.isi","000403274700035"],["dc.identifier.pmid","28609462"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14556"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/42326"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","PUB_WoS_Import"],["dc.publisher","Public Library Science"],["dc.relation.issn","1932-6203"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0/"],["dc.title","Effects of conversion of native cerrado vegetation to pasture on soil hydro-physical properties, evapotranspiration and streamflow on the Amazonian agricultural frontier"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","4485"],["dc.bibliographiccitation.issue","7"],["dc.bibliographiccitation.journal","Water Air & Soil Pollution"],["dc.bibliographiccitation.lastpage","4494"],["dc.bibliographiccitation.volume","223"],["dc.contributor.author","Koehler, S."],["dc.contributor.author","Jungkunst, Hermann F."],["dc.contributor.author","Gutzler, C."],["dc.contributor.author","Herrera, R."],["dc.contributor.author","Gerold, Gerhard"],["dc.date.accessioned","2018-11-07T09:06:43Z"],["dc.date.available","2018-11-07T09:06:43Z"],["dc.date.issued","2012"],["dc.description.abstract","In the light of global change, the necessity to monitor atmospheric depositions that have relevant effects on ecosystems is ever increasing particularly for tropical sites. For this study, atmospheric ionic depositions were measured on tropical Central Sulawesi at remote sites with both a conventional bulk water collector system (BWS collector) and with a passive ion exchange resin collector system (IER collector). The principle of IER collector to fix all ionic depositions, i.e. anions and cations, has certain advantages referring to (1) post-deposition transformation processes, (2) low ionic concentrations and (3) low rainfall and associated particulate inputs, e.g. dust or sand. The ionic concentrations to be measured for BWS collectors may easily fall below detection limits under low deposition conditions which are common for tropical sites of low land use intensity. Additionally, BWS collections are not as independent from the amount of rain fallen as are IER collections. For this study, the significant differences between both collectors found for nearly all measured elements were partly correlated to the rainfall pattern, i.e. for calcium, magnesium, potassium and sodium. However, the significant differences were, in most cases, not highly relevant. More relevant differences between the systems were found for aluminium and nitrate (434-484 %). Almost five times higher values for nitrate clarified the advantage of the IER system particularly for low deposition rate which is one particularity of atmospheric ionic deposition in tropical sites of extensive land use. The monthly resolution of the IER data offers new insights into the temporal distribution of annual ionic depositions. Here, it did not follow the tropical rain pattern of a drier season within generally wet conditions."],["dc.description.sponsorship","German Research Foundation; Storma Laboratory, Palu, Indonesia"],["dc.identifier.doi","10.1007/s11270-012-1211-8"],["dc.identifier.isi","000307276400074"],["dc.identifier.pmid","22865942"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/8132"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/25616"],["dc.notes.intern","Merged from goescholar"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0049-6979"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.title","Atmospheric Ionic Deposition in Tropical Sites of Central Sulawesi Determined by Ion Exchange Resin Collectors and Bulk Water Collector"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Regional Environmental Change"],["dc.bibliographiccitation.lastpage","9"],["dc.bibliographiccitation.volume","18"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Couto, Eduardo Guimarães"],["dc.contributor.author","Madari, Beata Emoke"],["dc.contributor.author","Jungkunst, Hermann F."],["dc.contributor.author","Amorim, Ricardo Silva Santos"],["dc.contributor.author","Hohnwald, Stefan"],["dc.contributor.author","Klingler, Michael"],["dc.contributor.author","de Almeida Machado, Pedro Luiz Oliveira"],["dc.contributor.author","Schönenberg, Regine"],["dc.contributor.author","Nendel, Claas"],["dc.date.accessioned","2020-12-10T14:11:11Z"],["dc.date.available","2020-12-10T14:11:11Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.1007/s10113-017-1268-4"],["dc.identifier.eissn","1436-378X"],["dc.identifier.issn","1436-3798"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/15549"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/70994"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.notes.intern","Merged from goescholar"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","CC BY 4.0"],["dc.rights.uri","http://creativecommons.org/licenses/by/4.0"],["dc.title","Carbon-optimised land management strategies for southern Amazonia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.artnumber","1161"],["dc.bibliographiccitation.firstpage","1161"],["dc.bibliographiccitation.issue","10"],["dc.bibliographiccitation.journal","Remote Sensing"],["dc.bibliographiccitation.volume","11"],["dc.contributor.author","de Souza Mendes, Flávia"],["dc.contributor.author","Baron, Daniel"],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Liesenberg, Veraldo"],["dc.contributor.author","Erasmi, Stefan"],["dc.date.accessioned","2019-07-09T11:51:29Z"],["dc.date.accessioned","2020-05-11T13:22:28Z"],["dc.date.available","2019-07-09T11:51:29Z"],["dc.date.available","2020-05-11T13:22:28Z"],["dc.date.issued","2019"],["dc.description.abstract","Mapping vegetation types through remote sensing images has proved to be e ective, especially in large biomes, such as the Brazilian Cerrado, which plays an important role in the context of management and conservation at the agricultural frontier of the Amazon. We tested several combinations of optical and radar images to identify the four dominant vegetation types that are prevalent in the Cerrado area (i.e., cerrado denso, cerradão, gallery forest, and secondary forest). We extracted features from both sources of data such as intensity, grey level co-occurrence matrix, coherence, and polarimetric decompositions using Sentinel 2A, Sentinel 1A, ALOS-PALSAR 2 dual/full polarimetric, and TanDEM-X images during the dry and rainy season of 2017. In order to normalize the analysis of these features, we used principal component analysis and subsequently applied the Random Forest algorithm to evaluate the classification of vegetation types. During the dry season, the overall accuracy ranged from 48 to 83%, and during the dry and rainy seasons it ranged from 41 up to 82%. The classification using Sentinel 2A images during the dry season resulted in the highest overall accuracy and kappa values, followed by the classification that used images from all sensors during the dry and rainy season. Optical images during the dry season were su cient to map the di erent types of vegetation in our study area."],["dc.identifier.doi","10.3390/rs11101161"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/16135"],["dc.identifier.scopus","2-s2.0-85066761706"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/59955"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/65039"],["dc.identifier.url","http://www.scopus.com/inward/record.url?eid=2-s2.0-85066761706&partnerID=MN8TOARS"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.publisher","MDPI"],["dc.relation.eissn","2072-4292"],["dc.relation.issn","2072-4292"],["dc.rights","CC BY 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by/4.0"],["dc.subject.ddc","550"],["dc.title","Optical and SAR Remote Sensing Synergism for Mapping Vegetation Types in the Endangered Cerrado/Amazon Ecotone of Nova Mutum—Mato Grosso"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","307"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Botanical Sciences"],["dc.bibliographiccitation.volume","95"],["dc.contributor.author","Gómez-Díaz, Jorge A."],["dc.contributor.author","Krömer, Thorsten"],["dc.contributor.author","Carvajal-Hernández, Cesar I."],["dc.contributor.author","Gerold, Gerhard"],["dc.contributor.author","Heitkamp, Felix"],["dc.date.accessioned","2019-07-09T11:43:44Z"],["dc.date.available","2019-07-09T11:43:44Z"],["dc.date.issued","2017"],["dc.identifier.doi","10.17129/botsci.859"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/14670"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/58965"],["dc.notes.intern","Merged from goescholar"],["dc.rights","CC BY-NC 4.0"],["dc.rights.uri","https://creativecommons.org/licenses/by-nc/4.0"],["dc.title","Richness and distribution of herbaceous angiosperms along gradients of elevation and forest disturbance in central Veracruz, Mexico"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","217"],["dc.bibliographiccitation.journal","Advances in geosciences"],["dc.bibliographiccitation.lastpage","220"],["dc.bibliographiccitation.volume","6"],["dc.contributor.author","Leemhuis, C."],["dc.contributor.author","Gerold, G."],["dc.date.accessioned","2019-07-10T08:13:03Z"],["dc.date.available","2019-07-10T08:13:03Z"],["dc.date.issued","2006"],["dc.description.abstract","Precipitation anomalies caused by the warm phase (El Niño) of the ENSO cycle lead to a strong decrease of water resources in South-East Asia. The aim of this work is to study the impact of warm phase ENSO caused precipitation anomalies on the water balance of a mesoscale tropical catchment in Central Sulawesi, Indonesia using a scenario analysis. We applied statistically generated precipitation anomalies caused by warm phase ENSO events on a validated hydrological model of the Palu River catchment (2694 km2) to investigate the implications of the generated ENSO scenarios on the total annual water balance, the annual discharge regime and the discharge variability. Moreover we analysed the influence of various catchment characteristics during warm phase ENSO conditions on the discharge variability through a comparison of different sub-catchment types. The results of the scenario analysis proved a severe decline of the annual discharge rate during warm phase ENSO conditions and an increase of the overall discharge variability"],["dc.identifier.fs","127013"],["dc.identifier.ppn","571566790"],["dc.identifier.purl","https://resolver.sub.uni-goettingen.de/purl?gs-1/4389"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/61109"],["dc.language.iso","en"],["dc.notes.intern","Merged from goescholar"],["dc.relation.issn","1680-7359"],["dc.relation.orgunit","Fakultät für Geowissenschaften und Geographie"],["dc.rights","Goescholar"],["dc.rights.uri","https://goescholar.uni-goettingen.de/licenses"],["dc.subject.ddc","551"],["dc.subject.ddc","577"],["dc.title","The impact of the warm phase of ENSO (El Niño Southern Oscillation) events on water resource availability of tropical catchments in Central Sulawesi, Indonesia"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.version","published_version"],["dspace.entity.type","Publication"]]