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  • 1
    Monograph available for loan
    Monograph available for loan
    Cheltenham [u.a.] : Elgar
    Call number: PIK B 010-16-90322
    Description / Table of Contents: After a long period of suburbanization, cities have been in vogue again since the 1980s. But why are people prepared to spend far more money on a small house in the city centre than on a large house in the countryside - and why doesn't this apply to all cities? The authors of this book argue that the appeal of the city in the 21st century is not only determined by the production side of the economy, but also by the consumption side: its array of shops, cultural activities and, for example, an historic city centre. All these factors translate into a huge disparity in land prices as well as different wages for urban and rural citizens. This study maps out these variations, with an economic approach to spatial planning and an emphasis on land rents as a basis for cost-benefit analysis. The use of land prices as a reflection of the appreciation for urban amenities is an ideal measurement tool in the cost-benefit analyses for local investments and spatial planning policies, and sheds new light on the organisation of public administration. This accessible book will be of interest to geographers, economists and social scientists, as well as policymakers involved in urban planning, seeking an in-depth understanding of land prices and the increasing importance of cities in the 21st century
    Type of Medium: Monograph available for loan
    Pages: VII, 135 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 9781784717438 , 9781784717445 (electronic)
    Language: English
    Note: Contents: 1. The resurrection of the city -- 2. Land underneath the city -- 3. The dynamics of the Dutch system of cities -- 4. The production city -- 5. The consumer city -- 6. Land prices and governmental policy -- 7. Agglomeration benefits and spatial planning policy -- 8. Social cost-benefit analysis of an inner city transformation project -- 9. Agenda for the future
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Publication Date: 2019-04-02
    Description: Many workers are daily exposed to occupational agents like gases/fumes, mineral dust or biological dust, which could induce adverse health effects. Epigenetic mechanisms, such as DNA methylation, have been suggested to play a role. We therefore aimed to identify differentially methylated regions (DMRs) upon occupational exposures in never-smokers and investigated if these DMRs associated with gene expression levels. To determine the effects of occupational exposures independent of smoking, 903 never-smokers of the LifeLines cohort study were included. We performed three genome-wide methylation analyses (Illumina 450 K), one per occupational exposure being gases/fumes, mineral dust and biological dust, using robust linear regression adjusted for appropriate confounders. DMRs were identified using comb-p in Python. Results were validated in the Rotterdam Study (233 never-smokers) and methylation-expression associations were assessed using Biobank-based Integrative Omics Study data (n = 2802). Of the total 21 significant DMRs, 14 DMRs were associated with gases/fumes and 7 with mineral dust. Three of these DMRs were associated with both exposures (RPLP1 and LINC02169 (2×)) and 11 DMRs were located within transcript start sites of gene expression regulating genes. We replicated two DMRs with gases/fumes (VTRNA2-1 and GNAS) and one with mineral dust (CCDC144NL). In addition, nine gases/fumes DMRs and six mineral dust DMRs significantly associated with gene expression levels. Our data suggest that occupational exposures may induce differential methylation of gene expression regulating genes and thereby may induce adverse health effects. Given the millions of workers that are exposed daily to occupational exposures, further studies on this epigenetic mechanism and health outcomes are warranted.
    Print ISSN: 0964-6906
    Electronic ISSN: 1460-2083
    Topics: Biology , Medicine
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  • 3
  • 4
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    PANGAEA
    In:  Supplement to: Hofstede, Coen Matthijs; Christoffersen, Poul; Hubbard, Bryn; Doyle, Samuel H; Young, Tun Jan; Diez, Anja; Eisen, Olaf; Hubbard, Alun L (2018): Physical Conditions of Fast Glacier Flow: 2. Variable Extent of Anisotropic Ice and Soft Basal Sediment From Seismic Reflection Data Acquired on Store Glacier, West Greenland. Journal of Geophysical Research-Earth Surface, 123(2), 349-362, https://doi.org/10.1002/2017JF004297
    Publication Date: 2023-03-16
    Description: Added are 5 seismic reflection data sets of Store Glacier, a tide water glacier in West Greenland Uummannaq Fjord. Two crossing profiles were recorded, 20140513, along the ice flow and 20140514, across the ice flow.
    Keywords: AWI_Glac; File content; File format; File name; File size; Glaciology @ AWI; Seismic reflection profile; SEISREFL; Store_Glacier; Uniform resource locator/link to file; West Greenland
    Type: Dataset
    Format: text/tab-separated-values, 25 data points
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  • 5
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    PANGAEA
    In:  Supplement to: Diez, Anja; Eisen, Olaf; Hofstede, Coen Matthijs; Bohleber, Pascal; Polom, Ulrich (2013): Joint interpretation of explosive and vibroseismic surveys on cold firn for the investigation of ice properties. Annals of Glaciology, 54(64), 201-210, https://doi.org/10.3189/2013AoG64A200
    Publication Date: 2023-06-27
    Description: Two seismic surveys were carried out on the high-altitude glacier saddle, Colle Gnifetti, Monte Rosa, Italy/Switzerland. Explosive and vibroseismic sources were tested to explore the best way to generate seismic waves to deduce shallow and intermediate properties (〈100 m) of firn and ice. The explosive source (SISSY) excites strong surface and diving waves, degrading data quality for processing; no englacial reflections besides the noisy bed reflector are visible. However, the strong diving waves are analyzed to derive the density distribution of the firn pack, yielding results similar to a nearby ice core. The vibrator source (ElViS), used in both P- and SH-wave modes, produces detectable laterally coherent reflections within the firn and ice column. We compare these with ice-core and radar data. The SH-wave data are particularly useful in providing detailed, high-resolution information on firn and ice stratigraphy. Our analyses demonstrate the potential of seismic methods to determine physical properties of firn and ice, particularly density and potentially also crystal-orientation fabric.
    Keywords: Colle_Gnifetti_KCI; Colle Gnifetti, Monte Rosa, Swiss Alps; File content; File size; ICEDRILL; Ice drill; Method comment; Uniform resource locator/link to sgy data file
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Schaffer, Janin; Kanzow, Torsten; von Appen, Wilken-Jon; von Albedyll, Luisa; Arndt, Jan Erik; Roberts, David H (2020): Bathymetry constrains ocean heat supply to Greenland's largest glacier tongue. Nature Geoscience, 13(3), 227-231, https://doi.org/10.1038/s41561-019-0529-x
    Publication Date: 2023-11-24
    Description: As an update to the RTopo-2.0.1 data set (https://doi.org/10.1594/PANGAEA.856844), RTopo-2.0.4 contains new original bathymetry data for the Northeast Greenland continental shelf. In the Southern Ocean, we added the Rosier et al. (JGR Oceans, 2018) bathymetry grid below Filchner Ice Shelf. This work was supported in part through the Deutsche Forschungsgemeinschaft (DFG) within the Special Priority Program (SPP) 1889 "Regional Sea Level Change and Society" (grant OGreen79), the German Federal Ministry for Education and Research (BMBF) within the GROCE project (Grant 03F0778A), the Natural Environment Research Council (NERC) large grant "Ice shelves in a warming world: Filchner Ice Shelf System" (NE/L013770/1), the NERC project "Greenland in a warmer climate: What controls the advance & retreat of the NE Greenland Ice Stream" (Grant NE/N011228/1), and the Helmholtz Climate Initiative "Regional Climate Change" (REKLIM).
    Keywords: AWI_PhyOce; File format; File name; File size; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; Greenland in a warmer climate: What controls the advance & retreat of the NE Greenland Ice Stream; GROCE; Helmholtz-Verbund Regionale Klimaänderungen = Helmholtz Climate Initiative (Regional Climate Change); Ice shelves in a warming world: Filchner Ice Shelf System; NERC_FISS; NERC_Greenland; Physical Oceanography @ AWI; Priority Programme 1889 Regional Sea Level Change and Society; REKLIM; RTopo; RTopo-2; SPP1889; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
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  • 7
    Publication Date: 2024-01-30
    Description: A gridded bathymetry of the sea floor under Ekström Ice Shelf, Antarctica. The seismic data used to map the bathymetry were collected between 2010 and 2018, using two different seismic vibroseis sources. The same snow streamer was used for all data acquisition - a 1500 m long, 60 channel snow streamer, with 25 m group spacing. Each group contains eight gimballed P-wave SM-4, 14 Hz geo-phones. For each seismic profile, the reflection time of the sea floor horizon was identified. The data across all profiles was gridded and depth converted, using an ice velocity of 3601 m/s a sea-water velocity of 1451 m/s.
    Keywords: Bathymetry; Ekström; Ekstrom_Ice_Shelf; Ekström Ice Shelf; Ice shelf; MULT; Multiple investigations; seismic reflection; Sub-EIS-Obs; vibroseis
    Type: Dataset
    Format: image/tiff, 21.5 MBytes
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  • 8
    Publication Date: 2024-01-30
    Description: Sea floor depth under Ekström Ice Shelf, Antarctica - from seismic reflection profiles collected between 2010 and 2018. For each seismic profile, the reflection time of the sea floor and ice-shelf base was identified and the depth to the sea floor was calculated using an ice velocity of 3601 m/s a sea-water velocity of 1451 m/s. The depths are referenced to mean sea-level (geoid EIGEN-6C4 ). The seismic data used here were collected using two different seismic vibroseis sources. The same snow streamer was used for all data acquisition - a 1500 m long, 60 channel snow streamer, with 25 m group spacing. Each group contains eight gimballed P-wave SM-4, 14 Hz geo-phones. Please note these data are the point data used to create the gridded bathymetry product of the region, found here: doi:10.1594/PANGAEA.907951 Details of data acquisition and processing are given here: doi:10.1029/2019GL086187.
    Keywords: Bathymetry; Bed elevation; Corrected for surface elevation using the REMA model, re-reference to the EIGEN6C4 Geoid; Ekström; Ekstrom_Ice_Shelf; Ekström Ice Shelf; Ice shelf; LATITUDE; LONGITUDE; MULT; Multiple investigations; Number; seismic reflection; Sub-EIS-Obs; vibroseis
    Type: Dataset
    Format: text/tab-separated-values, 117684 data points
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  • 9
    Publication Date: 2024-04-20
    Description: Support Force Glacier (SFG) is a large ice stream feeding into the Filchner Ice Shelf. The active seismic survey is recorded at the sheet-shelf transition of SFG. We map the bed while grounded, the ocean cavity around a surface channel at the ice shelf and its counterpart at the base, the basal channel, and the seabed. The survey consists of 5 seismic reflection profiles, 2 along-flow profiles and 3 across-flow profiles. The 2.42GB seismic data were recorded with a 300 m long streamer consisting of 96 30Hz p-wave sensors. The sample rate is 0.5 ms, record length 3000 ms. The data is single fold, shot spacing is 150 m: line name: profile TC paper: direction: #shots: - 20170501 profile I along-flow 291 shots - 20170502 profile III across-flow 28 shots - 20170503 profile II along-flow 71 shots - 20170504 profile IV across-flow 40 shots - 20170506 profile V across-flow 50 shots Presented are for each line (20170501 used as example): - The raw shots: 20170501_RAW_SHOTS_EDITS_GEOM.segy - The Kirchhoff migrated and depth converted profiles: 20170501stat_TXmig_Zconv.segy - The shot x,y,z coordinates in longitude, latitude and surface height in meters above sea level (z, WGS84 ellipsoid): 20170501_GPS.txt
    Keywords: 300 m snow streamer with 96 gimballed 30 Hz vertical compressional wave (P-wave) sensors; ANT-Land_2016/17_FISP; AWI Antarctic Land Expedition; Binary Object; Binary Object (File Size); Event label; Filchner Ice Shelf Project; File content; FISP; FISP_2016-2017_20170501; FISP_2016-2017_20170502; FISP_2016-2017_20170503; FISP_2016-2017_20170504; FISP_2016-2017_20170506; Ice-shelf Channels; profile I; profile II; profile III; profile IV; profile V; Snow streamer; SSTREAM
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
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  • 10
    Publication Date: 2024-04-20
    Description: To check the possible presence of a subglacial lake in Isunnguata Sermia, West Greenland we collected two 5 km perpendicular profiles of seismic reflection data. The data revealed a 1.9 km by 450 m and 50 m thick lens-shaped body at the bottom of a subglacial 190 m deep trough, most likely consisting of stratified consolidated sediments possibly overlain by dilatant till. Liquid water seems present at the northern and eastern flank of the subglacial trough. The bed on the northern side of the trough consists of unconsolidated, possibly water containing sediments, whereas on the southern side it consists of more consolidated material.
    Keywords: AWI-20130521; AWI-20130522; AWI-20130532; Binary Object; Binary Object (File Size); Comment; Event label; File content; ice2sea; Profile; Seismic reflection profile; SEISREFL
    Type: Dataset
    Format: text/tab-separated-values, 46 data points
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