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  • Abies; Acer; Achillea-type; AGE; Alchemilla; Alisma; Alnus; Apiaceae; Armeria; Artemisia; Asteraceae Liguliflorae; Aster-type; Batrachium-type; Betula; Boraginaceae; Botryococcus; Brassicaceae; Bryophyta undifferentiated; Calluna; Campanulaceae; Carpinus; Caryophyllaceae undifferentiated; Centaurea cyanus; Cerastium-type; Cerealia-type; Chenopodiaceae; Cirsium-type; Coelastrum; Corylus; Counting, palynology; Crassulaceae; Cyperaceae; DEPTH, sediment/rock; Dinoflagellates; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Ericaceae undifferentiated; Europe; Fabaceae; Fagus; Filicopsida undifferentiated; Filipendula; Fraxinus; Galium; Haemelsee_Haem13; Helianthemum nummularium-type; Helianthemum oelandicum-type; Hippophae; Hippuris vulgaris; Humulus/Cannabis-type; Hydrocharis-type; Ilex; Isoetes; Juglans; Juniperus; Lake Haemelsee, Germany; Lamiaceae; Late-Glacial; Liliaceae; Liquidambar; Lycopodium (added); Lycopodium annotinum-type; Lysimachia; Lythrum; Mentha-type; Menyanthes; Myriophyllum alterniflorum; Myriophyllum spicatum; Myriophyllum verticillatum; Niederreiter Piston corer; NPC; Number; Nuphar; Nymphaea; Palaeoecology; Parnassia palustris; Pediastrum; Picea; Pinus; Plantago lanceolata; Plantago maritima-type; Plantago media/major-type; Poaceae; Polemonium boreale; pollen; Pollen, undifferentiated; Polygonum aviculare-type; Polygonum persicaria/amphibia-type; Polypodium-type; Populus; Potamogeton; Potentilla-type; Pteridium; Quercus; Ranunculaceae undifferentiated; Ranunculus repens-type; Rosaceae undifferentiated; Rotatoria; Rumex; Rumex hydrolapathum; Salix; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Scrophulariaceae undifferentiated; Selaginella selaginoides; Silene-type; Succisa-type; Thalictrum; Tilia; Typha angustifolia/Sparganium-type; Typha latifolia-type; Ulmus; Urtica; Utricularia; Vaccinium; Valeriana; Vegetation change  (1)
  • Hurricane Harvey  (1)
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  • 1
    Publication Date: 2024-04-17
    Description: This dataset provides the raw pollen counts for the late-glacial sediment sequence retrieved from Lake Haemelsee (Germany) in 2013. The counts are presented against both depth (cm core depth) and time (cal. yr BP) and cover the time interval from ca 15.200 to 10.400 cal yr BP. A total of 106 samples were counted, with higher sampling resolution around the onset and end of the Younger Dryas, and lower sampling resolution elsewhere in the core. The pollen record provides information about both regional vegetation change as well as changes in the within-lake flora. It was produced to inform on the exact age and duration of major palynological transitions during the late-glacial Cores were retrieved from the lake using a 3-m long UWITEC piston corer deployed from a floating coring platform during field work in July 2013. Volumetric samples were obtained from splits of the core and processed in the laboratory (University of Amsterdam, the Netherlands) using standard protocols.
    Keywords: Abies; Acer; Achillea-type; AGE; Alchemilla; Alisma; Alnus; Apiaceae; Armeria; Artemisia; Asteraceae Liguliflorae; Aster-type; Batrachium-type; Betula; Boraginaceae; Botryococcus; Brassicaceae; Bryophyta undifferentiated; Calluna; Campanulaceae; Carpinus; Caryophyllaceae undifferentiated; Centaurea cyanus; Cerastium-type; Cerealia-type; Chenopodiaceae; Cirsium-type; Coelastrum; Corylus; Counting, palynology; Crassulaceae; Cyperaceae; DEPTH, sediment/rock; Dinoflagellates; Empetrum; Ephedra distachya-type; Ephedra fragilis-type; Epilobium; Equisetum; Ericaceae undifferentiated; Europe; Fabaceae; Fagus; Filicopsida undifferentiated; Filipendula; Fraxinus; Galium; Haemelsee_Haem13; Helianthemum nummularium-type; Helianthemum oelandicum-type; Hippophae; Hippuris vulgaris; Humulus/Cannabis-type; Hydrocharis-type; Ilex; Isoetes; Juglans; Juniperus; Lake Haemelsee, Germany; Lamiaceae; Late-Glacial; Liliaceae; Liquidambar; Lycopodium (added); Lycopodium annotinum-type; Lysimachia; Lythrum; Mentha-type; Menyanthes; Myriophyllum alterniflorum; Myriophyllum spicatum; Myriophyllum verticillatum; Niederreiter Piston corer; NPC; Number; Nuphar; Nymphaea; Palaeoecology; Parnassia palustris; Pediastrum; Picea; Pinus; Plantago lanceolata; Plantago maritima-type; Plantago media/major-type; Poaceae; Polemonium boreale; pollen; Pollen, undifferentiated; Polygonum aviculare-type; Polygonum persicaria/amphibia-type; Polypodium-type; Populus; Potamogeton; Potentilla-type; Pteridium; Quercus; Ranunculaceae undifferentiated; Ranunculus repens-type; Rosaceae undifferentiated; Rotatoria; Rumex; Rumex hydrolapathum; Salix; Sanguisorba minor; Sanguisorba officinalis; Saussurea-type; Scrophulariaceae undifferentiated; Selaginella selaginoides; Silene-type; Succisa-type; Thalictrum; Tilia; Typha angustifolia/Sparganium-type; Typha latifolia-type; Ulmus; Urtica; Utricularia; Vaccinium; Valeriana; Vegetation change
    Type: Dataset
    Format: text/tab-separated-values, 11978 data points
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  • 2
    Publication Date: 2021-04-22
    Description: Pluvial flood risk is mostly excluded in urban flood risk assessment. However, the risk of pluvial flooding is a growing challenge with a projected increase of extreme rainstorms compounding with an ongoing global urbanization. Considered as a flood type with minimal impacts when rainfall rates exceed the capacity of urban drainage systems, the aftermath of rainfall‐triggered flooding during Hurricane Harvey and other events show the urgent need to assess the risk of pluvial flooding. Due to the local extent and small‐scale variations, the quantification of pluvial flood risk requires risk assessments on high spatial resolutions. While flood hazard and exposure information is becoming increasingly accurate, the estimation of losses is still a poorly understood component of pluvial flood risk quantification. We use a new probabilistic multivariable modeling approach to estimate pluvial flood losses of individual buildings, explicitly accounting for the associated uncertainties. Except for the water depth as the common most important predictor, we identified the drivers for having loss or not and for the degree of loss to be different. Applying this approach to estimate and validate building structure losses during Hurricane Harvey using a property level data set, we find that the reliability and dispersion of predictive loss distributions vary widely depending on the model and aggregation level of property level loss estimates. Our results show that the use of multivariable zero‐inflated beta models reduce the 90% prediction intervalsfor Hurricane Harvey building structure loss estimates on average by 78% (totalling U.S.$3.8 billion) compared to commonly used models.
    Description: Key Points Recent severe pluvial flood events highlight the need to integrate pluvial flooding in urban flood risk assessment Probabilistic models provide reliable estimation of pluvial flood loss across spatial scales Beta distribution model reduces the 90% prediction interval for Hurricane Harvey building loss by U.S.$3.8 billion or 78%
    Description: Bundesministerium für Bildung und Forschung (BMBF) http://dx.doi.org/10.13039/501100002347
    Description: NSF GRFP
    Description: Fulbright Doctoral Program
    Keywords: 551.5 ; pluvial flooding ; loss modeling ; urban flooding ; probabilistic ; Hurricane Harvey ; climate change adaptation
    Type: article
    Location Call Number Expected Availability
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