@phdthesis{Pusch2012, author = {Pusch, Martin}, title = {Horizontale und vertikale Konnektivit{\"a}t in Fließgew{\"a}ssern und Seen : {\"o}kologische Funktionen und anthropogene {\"U}berformung}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-63713}, school = {Universit{\"a}t Potsdam}, year = {2012}, abstract = {Gew{\"a}sser werden traditionellerweise als abgeschlossene {\"O}kosysteme gesehen, und insbeson¬dere das Zirkulieren von Wasser und N{\"a}hrstoffen im Pelagial von Seen wird als Beispiel daf{\"u}r angef{\"u}hrt. Allerdings wurden in der j{\"u}ngeren Vergangenheit wichtige Verkn{\"u}pfungen des Freiwasserk{\"o}rpers von Gew{\"a}ssern aufgezeigt, die einerseits mit dem Benthal und andererseits mit dem Litoral, der terrestrischen Uferzone und ihrem Einzugsgebiet bestehen. Dadurch hat in den vergangen Jahren die horizontale und vertikale Konnektivit{\"a}t der Gew{\"a}sser{\"o}kosysteme erh{\"o}htes wissenschaftliches Interesse auf sich gezogen, und damit auch die {\"o}kologischen Funktionen des Gew{\"a}ssergrunds (Benthal) und der Uferzonen (Litoral). Aus der neu beschriebenen Konnektivit{\"a}t innerhalb und zwischen diesen Lebensr{\"a}umen ergeben sich weitreichende Konsequenzen f{\"u}r unser Bild von der Funktionalit{\"a}t der Gew{\"a}sser. In der vorliegenden Habilitationsschrift wird am Beispiel von Fließgew{\"a}ssern und Seen des nordostdeutschen Flachlandes eine Reihe von internen und externen funktionalen Verkn{\"u}pfungen in den horizontalen und vertikalen r{\"a}umlichen Dimensionen aufgezeigt. Die zugrunde liegenden Untersuchungen umfassten zumeist sowohl abiotische als auch biologische Variablen, und umfassten thematisch, methodisch und hinsichtlich der Untersuchungsgew{\"a}sser ein breites Spektrum. Dabei wurden in Labor- und Feldexperimenten sowie durch quantitative Feldmes¬sungen {\"o}kologischer Schl{\"u}sselprozesse wie N{\"a}hrstoffretention, Kohlenstoffumsatz, extrazellu¬l{\"a}re Enzymaktivit{\"a}t und Ressourcenweitergabe in Nahrungsnetzen (mittels Stabilisotopen¬methode) untersucht. In Bezug auf Fließgew{\"a}sser wurden dadurch wesentliche Erkenntnisse hinsichtlich der Wirkung einer durch Konnekticit{\"a}t gepr{\"a}gten Hydromorphologie auf die die aquatische Biodiversit{\"a}t und die benthisch-pelagische Kopplung erbracht, die wiederum einen Schl{\"u}sselprozess darstellt f{\"u}r die Retention von in der fließenden Welle transportierten Stoffen, und damit letztlich f{\"u}r die Produktivit{\"a}t eines Flussabschnitts. Das Litoral von Seen wurde in Mitteleuropa jahrzehntelang kaum untersucht, so dass die durchgef{\"u}hrten Untersuchungen zur Gemeinschaftsstruktur, Habitatpr{\"a}ferenzen und Nahrungs¬netzverkn{\"u}pfungen des eulitoralen Makrozoobenthos grundlegend neue Erkenntnisse erbrach¬ten, die auch unmittelbar in Ans{\"a}tze zur {\"o}kologischen Bewertung von Seeufern gem{\"a}ß EG-Wasserrahmenrichtlinie eingehen. Es konnte somit gezeigt werden, dass die Intensit{\"a}t sowohl die internen als auch der externen {\"o}kologischen Konnektivit{\"a}t durch die Hydrologie und Morphologie der Gew{\"a}sser sowie durch die Verf{\"u}gbarkeit von N{\"a}hrstoffen wesentlich beeinflusst wird, die auf diese Weise vielfach die {\"o}kologische Funktionalit{\"a}t der Gew{\"a}sser pr{\"a}gen. Dabei tr{\"a}gt die vertikale oder horizontale Konnektivit{\"a}t zur Stabilisierung der beteiligten {\"O}kosysteme bei, indem sie den Austausch erm{\"o}glicht von Pflanzenn{\"a}hrstoffen, von Biomasse sowie von migrierenden Organismen, wodurch Phasen des Ressourcenmangels {\"u}berbr{\"u}ckt werden. Diese Ergebnisse k{\"o}nnen im Rahmen der Bewirtschaftung von Gew{\"a}ssern dahingehend genutzt werden, dass die Gew{\"a}hrleistung horizontaler und vertikaler Konnektivit{\"a}t in der Regel mit r{\"a}umlich komplexeren, diverseren, zeitlich und strukturell resilienteren sowie leistungsf{\"a}hi¬geren {\"O}kosystemen einhergeht, die somit intensiver und sicherer nachhaltig genutzt werden k{\"o}nnen. Die Nutzung einer kleinen Auswahl von {\"O}kosystemleistungen der Fl{\"u}sse und Seen durch den Menschen hat oftmals zu einer starken Reduktion der {\"o}kologischen Konnektivit{\"a}t, und in der Folge zu starken Verlusten bei anderen {\"O}kosystemleistungen gef{\"u}hrt. Die Ergebnisse der dargestellten Forschungen zeigen auch, dass die Entwicklung und Implementierung von Strategien zum integrierten Management von komplexen sozial-{\"o}kologischen Systemen wesentlich unterst{\"u}tzt werden kann, wenn die horizontale und vertikale Konnektivit{\"a}t gezielt entwickelt wird.}, language = {de} } @article{PilzDelgadoVossetal.2019, author = {Pilz, Tobias and Delgado, Jos{\´e} Miguel Martins and Voss, Sebastian and Vormoor, Klaus Josef and Francke, Till and Cunha Costa, Alexandre and Martins, Eduardo and Bronstert, Axel}, title = {Seasonal drought prediction for semiarid northeast Brazil}, series = {Hydrology and Earth System Sciences}, volume = {23}, journal = {Hydrology and Earth System Sciences}, publisher = {Copernicus Publications}, address = {G{\"o}ttingen}, issn = {1027-5606}, doi = {10.5194/hess-23-1951-2019}, pages = {1951 -- 1971}, year = {2019}, abstract = {The semiarid northeast of Brazil is one of the most densely populated dryland regions in the world and recurrently affected by severe droughts. Thus, reliable seasonal forecasts of streamflow and reservoir storage are of high value for water managers. Such forecasts can be generated by applying either hydrological models representing underlying processes or statistical relationships exploiting correlations among meteorological and hydrological variables. This work evaluates and compares the performances of seasonal reservoir storage forecasts derived by a process-based hydrological model and a statistical approach. Driven by observations, both models achieve similar simulation accuracies. In a hindcast experiment, however, the accuracy of estimating regional reservoir storages was considerably lower using the process-based hydrological model, whereas the resolution and reliability of drought event predictions were similar by both approaches. Further investigations regarding the deficiencies of the process-based model revealed a significant influence of antecedent wetness conditions and a higher sensitivity of model prediction performance to rainfall forecast quality. Within the scope of this study, the statistical model proved to be the more straightforward approach for predictions of reservoir level and drought events at regionally and monthly aggregated scales. However, for forecasts at finer scales of space and time or for the investigation of underlying processes, the costly initialisation and application of a process-based model can be worthwhile. Furthermore, the application of innovative data products, such as remote sensing data, and operational model correction methods, like data assimilation, may allow for an enhanced exploitation of the advanced capabilities of process-based hydrological models.}, language = {en} } @misc{PilzDelgadoVossetal.2019, author = {Pilz, Tobias and Delgado, Jos{\´e} Miguel Martins and Voss, Sebastian and Vormoor, Klaus Josef and Francke, Till and Cunha Costa, Alexandre and Martins, Eduardo and Bronstert, Axel}, title = {Seasonal drought prediction for semiarid northeast Brazil}, series = {Postprints der Universit{\"a}t Potsdam Mathematisch-Naturwissenschaftliche Reihe}, journal = {Postprints der Universit{\"a}t Potsdam Mathematisch-Naturwissenschaftliche Reihe}, number = {702}, issn = {1866-8372}, doi = {10.25932/publishup-42795}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-427950}, pages = {21}, year = {2019}, abstract = {The semiarid northeast of Brazil is one of the most densely populated dryland regions in the world and recurrently affected by severe droughts. Thus, reliable seasonal forecasts of streamflow and reservoir storage are of high value for water managers. Such forecasts can be generated by applying either hydrological models representing underlying processes or statistical relationships exploiting correlations among meteorological and hydrological variables. This work evaluates and compares the performances of seasonal reservoir storage forecasts derived by a process-based hydrological model and a statistical approach. Driven by observations, both models achieve similar simulation accuracies. In a hindcast experiment, however, the accuracy of estimating regional reservoir storages was considerably lower using the process-based hydrological model, whereas the resolution and reliability of drought event predictions were similar by both approaches. Further investigations regarding the deficiencies of the process-based model revealed a significant influence of antecedent wetness conditions and a higher sensitivity of model prediction performance to rainfall forecast quality. Within the scope of this study, the statistical model proved to be the more straightforward approach for predictions of reservoir level and drought events at regionally and monthly aggregated scales. However, for forecasts at finer scales of space and time or for the investigation of underlying processes, the costly initialisation and application of a process-based model can be worthwhile. Furthermore, the application of innovative data products, such as remote sensing data, and operational model correction methods, like data assimilation, may allow for an enhanced exploitation of the advanced capabilities of process-based hydrological models.}, language = {en} } @article{MedeirosdeAraujoMamedeetal.2014, author = {Medeiros, Pedro Henrique Augusto and de Araujo, Jose Carlos and Mamede, George Leite and Creutzfeldt, Benjamin and Guentner, Andreas and Bronstert, Axel}, title = {Connectivity of sediment transport in a semiarid environment: a synthesis for the Upper Jaguaribe Basin, Brazil}, series = {Journal of soils and sediments : protection, risk assessment and remediation}, volume = {14}, journal = {Journal of soils and sediments : protection, risk assessment and remediation}, number = {12}, publisher = {Springer}, address = {Heidelberg}, issn = {1439-0108}, doi = {10.1007/s11368-014-0988-z}, pages = {1938 -- 1948}, year = {2014}, abstract = {Hydrosedimentological studies conducted in the semiarid Upper Jaguaribe Basin, Brazil, enabled the identification of the key processes controlling sediment connectivity at different spatial scales (10(0)-10(4) km(2)). Water and sediment fluxes were assessed from discharge, sediment concentrations and reservoir siltation measurements. Additionally, mathematical modelling (WASA-SED model) was used to quantify water and sediment transfer within the watershed. Rainfall erosivity in the study area was moderate (4600 MJ mm ha(-1) h(-1) year(-1)), whereas runoff depths (16-60 mm year(-1)), and therefore the sediment transport capacity, were low. Consequently, similar to 60 \% of the eroded sediment was deposited along the landscape, regardless of the spatial scale. The existing high-density reservoir network (contributing area of 6 km(2) per reservoir) also limits sediment propagation, retaining up to 47 \% of the sediment at the large basin scale. The sediment delivery ratio (SDR) decreased with the spatial scale; on average, 41 \% of the eroded sediment was yielded from the hillslopes, while for the whole 24,600-km(2) basin, the SDR was reduced to 1 \% downstream of a large reservoir (1940-hm(3) capacity). Hydrological behaviour in the Upper Jaguaribe Basin represents a constraint on sediment propagation; low runoff depth is the main feature breaking sediment connectivity, which limits sediment transference from the hillslopes to the drainage system. Surface reservoirs are also important barriers, but their relative importance to sediment retention increases with scale, since larger contributing areas are more suitable for the construction of dams due to higher hydrological potential.}, language = {en} } @article{MayGiladiRistowetal.2013, author = {May, Felix and Giladi, Itamar and Ristow, Michael and Ziv, Yaron and Jeltsch, Florian}, title = {Plant functional traits and community assembly along interacting gradients of productivity and fragmentation}, series = {Perspectives in plant ecology, evolution and systematics}, volume = {15}, journal = {Perspectives in plant ecology, evolution and systematics}, number = {6}, publisher = {Elsevier}, address = {Jena}, issn = {1433-8319}, doi = {10.1016/j.ppees.2013.08.002}, pages = {304 -- 318}, year = {2013}, abstract = {Quantifying the association of plant functional traits to environmental gradients is a promising approach for understanding and projecting community responses to land use and climatic changes. Although habitat fragmentation and climate are expected to affect plant communities interactively, there is a lack of empirical studies addressing trait associations to fragmentation in different climatic regimes. In this study, we analyse data on the key functional traits: specific leaf area (SLA), plant height, seed mass and seed number. First, we assess the evidence for the community assembly mechanisms habitat filtering and competition at different spatial scales, using several null-models and a comprehensive set of community-level trait convergence and divergence indices. Second, we analyse the association of community-mean traits with patch area and connectivity along a south-north productivity gradient. We found clear evidence for trait convergence due to habitat filtering. In contrast, the evidence for trait divergence due to competition fundamentally depended on the null-model used. When the null-model controlled for habitat filtering, there was only evidence for trait divergence at the smallest sampling scale (0.25 m x 0.25 m). All traits varied significantly along the S-N productivity gradient. While plant height and SLA were consistently associated with fragmentation, the association of seed mass and seed number with fragmentation changed along the S-N gradient. Our findings indicate trait convergence due to drought stress in the arid sites and due to higher productivity in the mesic sites. The association of plant traits to fragmentation is likely driven by increased colonization ability in small and/or isolated patches (plant height, seed number) or increased persistence ability in isolated patches (seed mass). Our study provides the first empirical test of trait associations with fragmentation along a productivity gradient. We conclude that it is crucial to study the interactive effects of different ecological drivers on plant functional traits.}, language = {en} } @article{HolzBuchmannBoeckerSchlieretal.2015, author = {Holz, Nathalie E. and Buchmann, Arlette F. and Boecker-Schlier, Regina and Blomeyer, Dorothea and Baumeister, Sarah and Wolf, Isabella and Rietschel, Marcella and Witt, Stephanie H. and Plichta, Michael M. and Meyer-Lindenberg, Andreas and Banaschewski, Tobias and Brandeis, Daniel and Laucht, Manfred}, title = {Role of FKBP5 in emotion processing: results on amygdala activity, connectivity and volume}, series = {Brain structure \& function}, volume = {220}, journal = {Brain structure \& function}, number = {3}, publisher = {Springer}, address = {Heidelberg}, issn = {1863-2653}, doi = {10.1007/s00429-014-0729-5}, pages = {1355 -- 1368}, year = {2015}, abstract = {Accumulating evidence suggests a role of FKBP5, a co-chaperone regulating the glucocorticoid receptor sensitivity, in the etiology of depression and anxiety disorders. Based on recent findings of altered amygdala activity following childhood adversity, the present study aimed at clarifying the impact of genetic variation in FKBP5 on threat-related neural activity and coupling as well as morphometric alterations in stress-sensitive brain systems. Functional magnetic resonance imaging during an emotional face-matching task was performed in 153 healthy young adults (66 males) from a high-risk community sample followed since birth. Voxel-based morphometry was applied to study structural alterations and DNA was genotyped for FKBP5 rs1360780. Childhood adversity was measured using retrospective self-report (Childhood Trauma Questionnaire) and by a standardized parent interview assessing childhood family adversity. Depression was assessed by the Beck Depression Inventory. There was a main effect of FKBP5 on the left amygdala, with T homozygotes showing the highest activity, largest volume and increased coupling with the left hippocampus and the orbitofrontal cortex (OFC). Moreover, amygdala-OFC coupling proved to be associated with depression in this genotype. In addition, our results support previous evidence of a gene-environment interaction on right amygdala activity with respect to retrospective assessment of childhood adversity, but clarify that this does not generalize to the prospective assessment. These findings indicated that activity in T homozygotes increased with the level of adversity, whereas the opposite pattern emerged in C homozygotes, with CT individuals being intermediate. The present results point to a functional involvement of FKBP5 in intermediate phenotypes associated with emotional processing, suggesting a possible mechanism for this gene in conferring susceptibility to stress-related disorders.}, language = {en} } @article{GroschwitzSzabo2017, author = {Groschwitz, Jonas and Szabo, Tibor}, title = {Sharp Thresholds for Half-Random Games II}, series = {GRAPHS AND COMBINATORICS}, volume = {33}, journal = {GRAPHS AND COMBINATORICS}, publisher = {Springer}, address = {Tokyo}, issn = {0911-0119}, doi = {10.1007/s00373-016-1753-4}, pages = {387 -- 401}, year = {2017}, abstract = {We study biased Maker-Breaker positional games between two players, one of whom is playing randomly against an opponent with an optimal strategy. In this work we focus on the case of Breaker playing randomly and Maker being "clever". The reverse scenario is treated in a separate paper. We determine the sharp threshold bias of classical games played on the edge set of the complete graph , such as connectivity, perfect matching, Hamiltonicity, and minimum degree-1 and -2. In all of these games, the threshold is equal to the trivial upper bound implied by the number of edges needed for Maker to occupy a winning set. Moreover, we show that CleverMaker can not only win against asymptotically optimal bias, but can do so very fast, wasting only logarithmically many moves (while the winning set sizes are linear in n).}, language = {en} } @article{BronstertdeAraujoBatallaVillanuevaetal.2014, author = {Bronstert, Axel and de Araujo, Jose-Carlos and Batalla Villanueva, Ramon J. and Costa, Alexandre Cunha and Delgado, Jos{\´e} Miguel Martins and Francke, Till and F{\"o}rster, Saskia and Guentner, Andreas and Lopez-Tarazon, Jos{\´e} Andr{\´e}s and Mamede, George Leite and Medeiros, Pedro Henrique Augusto and Mueller, Eva and Vericat, Damia}, title = {Process-based modelling of erosion, sediment transport and reservoir siltation in mesoscale semi-arid catchments}, series = {Journal of soils and sediments : protection, risk assessment and remediation}, volume = {14}, journal = {Journal of soils and sediments : protection, risk assessment and remediation}, number = {12}, publisher = {Springer}, address = {Heidelberg}, issn = {1439-0108}, doi = {10.1007/s11368-014-0994-1}, pages = {2001 -- 2018}, year = {2014}, abstract = {To support scientifically sound water management in dryland environments a modelling system has been developed for the quantitative assessment of water and sediment fluxes in catchments, transport in the river system, and retention in reservoirs. The spatial scale of interest is the mesoscale because this is the scale most relevant for management of water and land resources. This modelling system comprises process-oriented hydrological components tailored for dryland characteristics coupled with components comprising hillslope erosion, sediment transport and reservoir deposition processes. The spatial discretization is hierarchically designed according to a multi-scale concept to account for particular relevant process scales. The non-linear and partly intermittent run-off generation and sediment dynamics are dealt with by accounting for connectivity phenomena at the intersections of landscape compartments. The modelling system has been developed by means of data from nested research catchments in NE-Spain and in NE-Brazil. In the semi-arid NE of Brazil sediment retention along the topography is the main process for sediment retention at all scales, i.e. the sediment delivery is transport limited. This kind of deposition retains roughly 50 to 60 \% of eroded sediment, maintaining a similar deposition proportion in all spatial scales investigated. On the other hand, the sediment retained in reservoirs is clearly related to the scale, increasing with catchment area. With increasing area, there are more reservoirs, increasing the possibility of deposition. Furthermore, the area increase also promotes an increase in flow volume, favouring the construction of larger reservoirs, which generally overflow less frequently and retain higher sediment fractions. The second example comprises a highly dynamic Mediterranean catchment in NE-Spain with nested sub-catchments and reveals the full dynamics of hydrological, erosion and deposition features. The run-off modelling performed well with only some overestimation during low-flow periods due to the neglect of water losses along the river. The simulated peaks in sediment flux are reproduced well, while low-flow sediment transport is less well captured, due to the disregard of sediment remobilization in the riverbed during low flow. This combined observation and modelling study deepened the understanding of hydro-sedimentological systems characterized by flashy run-off generation and by erosion and sediment transport pulses through the different landscape compartments. The connectivity between the different landscape compartments plays a very relevant role, regarding both the total mass of water and sediment transport and the transport time through the catchment.}, language = {en} }