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  • 1
    Monograph available for loan
    Monograph available for loan
    Wallingford : IAHS Press
    Call number: PIK N 454-09-0112
    Type of Medium: Monograph available for loan
    Pages: XIII, 343 S. : Ill., graph. Darst.
    ISBN: 9781901502541
    Series Statement: IAHS special publication 8
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Call number: AWI G1-02-0088
    In: Developments in plant and soil sciences, Volume 88
    Description / Table of Contents: Environmental studies typically involve the combination of dynamic models with data sources at various spatial and temporal scales. Also, the scale of the model output is rarely in tune with the scale at which decision-makers require answers or implement environmental measures. Consequently, the question has been raised how to obtain results at the appropriate scale. Models, usually developed at the scale of a research project, have to be applied to larger areas (extrapolation), with incomplete data coverage (interpolation) and to different supports (upscaling and downscaling) to facilitate studies for decision-makers. This book gives an overview of the various problems involved, and focuses on a description of upscaling and downscaling methods that are known to exist. Furthermore, this book is the first in its kind in that it contains a decision support system that advises the practitioner on which upscaling or downscaling method to use in his specific context. This book is meant for an audience of MSc- and PhD-students, applied researchers and practitioners in soil science, hydrology, (agro) ecology, agronomy and the environmental sciences in general.
    Type of Medium: Monograph available for loan
    Pages: X, 190 Seiten , Illustrationen
    ISBN: 0-7923-6339-6
    Series Statement: Developments in plant and soil sciences 88
    Language: English
    Note: Contents Preface 1. Introduction 1.1 The problem of scale transfer 1.2 Aims and scope 1.3 Definitions 1.4 Contents of this book 2. Upscaling 2.1 A classification of upscaling methods 2.2 Averaging of observations or output variables 2.2.1 Exhaustive Information 2.2.2 Design based methods 2.2.3 Geostatistical prediction 2.2.4 Deterministic functions 2.2.5 Combinations and auxiliary information 2.3 Finding representative parameters or input variables 2.3.1 Exhaustive information 2.3.2 Deterministic functions 2.3.3 Indirect stochastic methods 2.3.4 Direct stochastic methods 2.3.5 Inverse modelling 2.4 Averaging of model equations 2.4.1 Deterministic: temporal or volume averaging 2.4.2 Stochastic: ensemble averaging 2.5 Model simplification 2.5.1 Lumped conceptual modelling 2.5.2 Meta-modelling 3. Downscaling 3.1 A classification of downscaling methods 3.2 Empirical functions 3.2.1 Deterministic functions 3.2.2 Conditional stochastic functions 3.2.3 Unconditional stochastic functions 3.3 Mechanistic models 3.3.1 Deterministic functions 3.3.2 Conditional stochastic functions 3.3.3 Unconditional stochastic functions 3.4 Fine scale auxiliary information 3.4.1 Deterministic functions 3.4.2 Conditional stochastic functions 3.4.3 Unconditional stochastic functions 4. A simple DSS for upscaling and downscaling 4.1 Purpose and philosophy of the DSS 4.2 Functionality and options at startup 4.3 Definition of the research chain over the scales 4.3.1 Define a new research chain 4.3.2 Modify parts of research chain 4.4 Enter the DSS from the research chain 4.5 DSS Upscaling and Downscaling Appendix: Random Variables and Stochastic Functions Glossary Contents References Index
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 3
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    PANGAEA
    In:  Supplement to: Zamrsky, Daniel; Oude Essink, Gualbert H P; Bierkens, Marc F P (2018): Estimating the thickness of unconsolidated coastal aquifers along the global coastline. Earth System Science Data, 10(3), 1591-1603, https://doi.org/10.5194/essd-10-1591-2018
    Publication Date: 2023-01-13
    Description: Information on aquifer thickness is one of the crucial inputs to numerical groundwater flow models, especially in the coastal areas that are threatened by increasing salt water intrusion leading to declining fresh groundwater resources. Since aquifer thickness data is missing in many parts of the world we designed a methodology to estimate it on global scale using state of the art datasets. We estimated the aquifer thickness by combining global topographical (Weatherhall et al., 2015, doi:10.1002/2015EA000107), lithological (Hartmann et. al, 2012, doi:10.1029/2012GC004370), soil thickness (Pelletier et al., 2016, doi:10.1002/2015MS000526) and sediment thickness from the global PCR-GLOBWB model (de Graaf et. al, 2015, doi:10.5194/hess-19-823-2015) to find the position and slope of the bedrock formation that are overlaid by unconsolidated sediments forming the aquifer system. The dataset includes the estimates of aquifer thickness at the coastline for each cross-section together with corresponding "anchor points" (last point with known thickness from Pelletier et. al, 2016). With this information it is possible to create 2D cross-sectional groundwater flow coupled with salt transport models to estimate the fresh groundwater resources in coastal areas. More attention should be paid to the composition of unconsolidated sediment aquifers in terms of low permeable layers that can play a large role in the distribution of fresh and saline groundwater.
    Type: Dataset
    Format: application/zip, 3.2 MBytes
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  • 4
    Publication Date: 2023-01-13
    Description: This dataset provides a consistent and comprehensive outlook of global wastewater production, collection, treatment and re-use at both the country-level and 5 arc-min resolution (gridded) for the year 2015. Country-level estimates of wastewater reported from various sources are used as basis, supplemented with predictions based on multiple linear regression using social, economic, hydrological and geographical predictor variables. Country-level wastewater data are provided in both volume flow rate (million m3 yr-1) and percentage terms. Wastewater data is downscaled to gridded (5 arc-min; m3 yr-1) estimates based on simulations of domestic and industrial return flows from the Water Futures and Solutions (WFaS; Wada et al., 2016) using the approach developed for PCRaster GlOBal Water Balance model (PCR-GLOBWB2; Sutanudjaja et al (2018)). Estimates of downscaled wastewater treatment and re-use are validated based on wastewater treatment plant capacities reported in various databases.
    Keywords: Municipal wastewater; PCR-GLOBWB; return flow; wastewater collection; Wastewater production; wastewater re-use; wastewater treatment; WFaS
    Type: Dataset
    Format: application/zip, 3.9 MBytes
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  • 5
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    PANGAEA
    In:  Supplement to: Gruber, Thomas; Bamber, Jonathan L; Bierkens, Marc F P; Dobslaw, Henryk; Murböck, M; Thomas, M; van Beek, L P H; van Dam, T; Vermeersen, L L A; Visser, P N A M (2011): Simulation of the time-variable gravity field by means of coupled geophysical models. Earth System Science Data, 3(1), 19-35, https://doi.org/10.5194/essd-3-19-2011
    Publication Date: 2023-09-02
    Description: Time variable gravity fields, reflecting variations of mass distribution in the system Earth is one of the key parameters to understand the changing Earth. Mass variations are caused either by redistribution of mass in, on or above the Earth's surface or by geophysical processes in the Earth's interior. The first set of observations of monthly variations of the Earth gravity field was provided by the US/German GRACE satellite mission beginning in 2002. This mission is still providing valuable information to the science community. However, as GRACE has outlived its expected lifetime, the geoscience community is currently seeking successor missions in order to maintain the long time series of climate change that was begun by GRACE. Several studies on science requirements and technical feasibility have been conducted in the recent years. These studies required a realistic model of the time variable gravity field in order to perform simulation studies on sensitivity of satellites and their instrumentation. This was the primary reason for the European Space Agency (ESA) to initiate a study on ''Monitoring and Modelling individual Sources of Mass Distribution and Transport in the Earth System by Means of Satellites''. The goal of this interdisciplinary study was to create as realistic as possible simulated time variable gravity fields based on coupled geophysical models, which could be used in the simulation processes in a controlled environment. For this purpose global atmosphere, ocean, continental hydrology and ice models were used. The coupling was performed by using consistent forcing throughout the models and by including water flow between the different domains of the Earth system. In addition gravity field changes due to solid Earth processes like continuous glacial isostatic adjustment (GIA) and a sudden earthquake with co-seismic and post-seismic signals were modelled. All individual model results were combined and converted to gravity field spherical harmonic series, which is the quantity commonly used to describe the Earth's global gravity field. The result of this study is a twelve-year time-series of 6-hourly time variable gravity field spherical harmonics up to degree and order 180 corresponding to a global spatial resolution of 1 degree in latitude and longitude. In this paper, we outline the input data sets and the process of combining these data sets into a coherent model of temporal gravity field changes. The resulting time series was used in some follow-on studies and is available to anybody interested.
    Keywords: DATE/TIME; File name; Method comment; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 180 data points
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  • 6
    Publication Date: 2018-01-22
    Description: Assessing reliability of global models is critical because of increasing reliance on these models to address past and projected future climate and human stresses on global water resources. Here, we evaluate model reliability based on a comprehensive comparison of decadal trends (2002–2014) in land water storage from seven global models (WGHM, PCR-GLOBWB, GLDAS NOAH, MOSAIC, VIC, CLM, and CLSM) to trends from three Gravity Recovery and Climate Experiment (GRACE) satellite solutions in 186 river basins (∼60% of global land area). Medians of modeled basin water storage trends greatly underestimate GRACE-derived large decreasing (≤−0.5 km3/y) and increasing (≥0.5 km3/y) trends. Decreasing trends from GRACE are mostly related to human use (irrigation) and climate variations, whereas increasing trends reflect climate variations. For example, in the Amazon, GRACE estimates a large increasing trend of ∼43 km3/y, whereas most models estimate decreasing trends (−71 to 11 km3/y). Land water storage trends, summed over all basins, are positive for GRACE (∼71–82 km3/y) but negative for models (−450 to −12 km3/y), contributing opposing trends to global mean sea level change. Impacts of climate forcing on decadal land water storage trends exceed those of modeled human intervention by about a factor of 2. The model-GRACE comparison highlights potential areas of future model development, particularly simulated water storage. The inability of models to capture large decadal water storage trends based on GRACE indicates that model projections of climate and human-induced water storage changes may be underestimated.
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 7
    Publication Date: 2020-04-29
    Print ISSN: 0043-1397
    Electronic ISSN: 1944-7973
    Topics: Architecture, Civil Engineering, Surveying , Geography
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  • 8
    Publication Date: 2017-02-17
    Print ISSN: 0049-6979
    Electronic ISSN: 1573-2932
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 9
  • 10
    Publication Date: 2019-12-19
    Description: Holocene marine transgressions are often put forward to explain observed groundwater salinities that extend far inland in deltas. This hypothesis was also proposed in the literature to explain the large land-inward extent of saline groundwater in the Nile Delta. The groundwater models previously built for the area used very large dispersivities to reconstruct this saline and brackish groundwater zone. However, this approach cannot explain the observed freshening of this zone. Here, we investigated the physical plausibility of the Holocene-transgression hypothesis to explain observed salinities by conducting a palaeohydrogeological reconstruction of groundwater salinity for the last 32 ka with a complex 3-D variable-density groundwater flow model, using a state-of-the-art version of the SEAWAT computer code that allows for parallel computation. Several scenarios with different lithologies and hypersaline groundwater provenances were simulated, of which five were selected that showed the best match with the observations. Amongst these selections, total freshwater volumes varied strongly, ranging from 1526 to 2659 km3, mainly due to uncertainties in the lithology offshore and at larger depths. This range is smaller (1511–1989 km3) when we only consider the volumes of onshore fresh groundwater within 300 m depth. In all five selected scenarios the total volume of hypersaline groundwater exceeded that of seawater. We also show that during the last 32 ka, total freshwater volumes significantly declined, with a factor ranging from 2 to 5, due to the rising sea level. Furthermore, the time period required to reach a steady state under current boundary conditions exceeded 5.5 ka for all scenarios. Finally, under highly permeable conditions the marine transgression simulated with the palaeohydrogeological reconstruction led to a steeper fresh–salt interface compared to its steady-state equivalent, while low-permeable clay layers allowed for the preservation of fresh groundwater volumes. This shows that long-term transient simulations are needed when estimating present-day fresh–salt groundwater distributions in large deltas. The insights of this study are also applicable to other major deltaic areas, since many also experienced a Holocene marine transgression.
    Print ISSN: 1027-5606
    Electronic ISSN: 1607-7938
    Topics: Geography , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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