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  • 2015-2019  (8,072)
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  • 1
    facet.materialart.12
    [Cham] : Springer
    Call number: 9783319595979 (e-book)
    Description / Table of Contents: This textbook introduces fundamental dynamics of tropical atmosphere and ocean useful for advanced graduate courses in atmospheric and climate sciences. It presents an overview of simple atmospheric and oceanic models, as well as the observed phenomena associated with major climate modes in the tropics. It provides students with an up-to-date understanding of the dynamics of tropical climate and weather phenomena. A particular focus is given to scale interactions and atmosphere-ocean interactions associated with tropical mean climate (such as ITCZ asymmetry and annual cycles), synoptic-scale variability (such as synoptic wave trains, easterly waves and tropical cyclones), intraseasonal oscillations (such as Madden-Julian Oscillation and boreal summer intraseasonal oscillation), and interannual variability (such as El Niño-Southern Oscillation and Indian Ocean Dipole). Theoretical and conceptual models are presented for better understanding of physical mechanisms behind the observational phenomena. This book aims to motivate graduate students in atmospheric sciences and oceanography by providing them with the key methods and tools necessary to conduct research.
    Type of Medium: 12
    Pages: 1 Online-Ressource (x, 229 Seiten) , Diagramme
    ISBN: 9783319595979 , 978-3-319-59597-9
    ISSN: 2194-5217 , 2194-5225
    Series Statement: Springer atmospheric sciences
    Language: English
    Note: Contents 1 Simple Dynamic Frameworks for Tropical Atmosphere and Ocean 1.1 Free Waves in an Equatorial Beta-Plane 1.2 Vertical Mode Separation in a Stratified Atmosphere 1.3 The Gill Model 1.4 The Lindzen–Nigam Model 1.5 The Cane–Zebiak Simple Coupled Atmosphere–Ocean Model 1.6 A 2.5-Layer Tropical Atmospheric Model 1.7 A 2.5-Layer Tropical Oceanic Model References 2 Roles of Air–Sea Interaction in Shaping Tropical Mean Climate 2.1 ITCZ Asymmetry 2.2 Theories 2.3 Effects of Asymmetric Land Mass and Coastal Geometry 2.4 Annual Cycle at the Equator References 3 Madden-Julian Oscillation: Observations and Mechanisms 3.1 Introduction 3.2 Observed Structure and Evolution Features 3.3 Mechanisms for Eastward Propagation 3.4 Initiation Mechanisms 3.5 Boreal Summer Intraseasonal Oscillation (BSISO) 3.6 Interactions with High-Frequency Eddies References 4 Tropical Cyclone Formation 4.1 Introduction 4.2 Precursor Synoptic Signals 4.3 Origin of Synoptic-Scale Wave Trains and Easterly Waves in WNP 4.4 Numerical Simulations of TC Genesis 4.5 MJO and ENSO Impacts 4.6 Projection of Future TC Changes Under Global Warming 4.7 Concluding Remark References 5 Dynamics of El Niño–Southern Oscillation 5.1 Observed Structure and Evolution 5.2 Instability Mechanisms 5.3 Oscillation Theories 5.4 Phase Locking to the Annual Cycle 5.5 El Niño and La Niña Amplitude Asymmetry 5.6 El Niño and La Niña Evolution Asymmetry 5.7 Modulation of Interdecadal Mean State on El Niño Behavior 5.8 Indian Ocean Dipole References 6 Monsoon Dynamics and Its Interactions with Ocean 6.1 Introduction 6.2 Theories on Tropospheric Biennial Oscillation (TBO) 6.3 Quasi-Biennial and Lower-Frequency Variability of the Monsoon 6.4 Pacific–East Asia Teleconnection 6.5 Effects of Indian Ocean and WNP SSTA on Circulation in WNP 6.6 Modulation of the Monsoon Mean Flow on El Niño Response 6.7 Inter-monsoon Relationships 6.8 Effect of Aerosol on Monsoon References
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  • 2
    Publication Date: 2018-05-05
    Description: IJERPH, Vol. 15, Pages 913: A Cross-Disciplinary Successful Aging Intervention and Evaluation: Comparison of Person-to-Person and Digital-Assisted Approaches International Journal of Environmental Research and Public Health doi: 10.3390/ijerph15050913 Authors: Hui-Chuan Hsu Tsuann Kuo Ju-Ping Lin Wei-Chung Hsu Chia-Wen Yu Yen-Cheng Chen Wan-Zhen Xie Wei-Chiang Hsu Ya-Lan Hsu Mu-Ting Yu Background: Successful aging has been the paradigm of old-age life. The purpose of this study was to implement and evaluate a cross-disciplinary intervention program using two approaches for community-based older adults in Taichung, Taiwan. Methods: The content of the intervention included successful aging concepts and preparation, physical activity, chronic disease and health management, dietary and nutrition information, cognitive training, emotional awareness and coping skills, family relationship and resilience, legal concepts regarding financial protection, and Internet use. The traditional person-to-person (P2P) intervention approach was implemented among participants at urban centers, and the personal-and-digital (P&D) intervention approach was implemented among participants at rural centers; before the P&D group received the intervention, participants were assessed as the control group for comparison. Results: Healthy behavior and nutrition improved for the P2P group, although not significantly. Strategies for adapting to old age and reducing ineffective coping were significantly improved in the P2P group. The ability to search for health information improved in the P&D group, and knowledge of finance-related law increased in the P2P group. Conclusion: A continuous, well-designed and evidence-based intervention program is beneficial for improving the health of older adults, or at least delaying its decline.
    Print ISSN: 1661-7827
    Electronic ISSN: 1660-4601
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Medicine
    Published by MDPI Publishing
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  • 3
    Publication Date: 2018-05-04
    Print ISSN: 1661-7827
    Electronic ISSN: 1660-4601
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Medicine
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Sahling, Heiko; Borowski, Christian; Escobar-Briones, Elva; Gaytán-Caballero, Adriana; Hsu, Chieh-Wei; Loher, Markus; MacDonald, Ian R; Marcon, Yann; Pape, Thomas; Römer, Miriam; Rubin-Blum, Maxim; Schubotz, Florence; Smrzka, Daniel; Wegener, Gunter; Bohrmann, Gerhard (2016): Massive asphalt deposits, oil seepage, and gas venting support abundant chemosynthetic communities at the Campeche Knolls, southern Gulf of Mexico. Biogeosciences, 13(15), 4491-4512, https://doi.org/10.5194/bg-13-4491-2016
    Publication Date: 2024-02-02
    Description: Hydrocarbon seepage is a widespread process at the continental margins of the Gulf of Mexico. We used a multidisciplinary approach, including multibeam mapping and visual seafloor observations with different underwater vehicles to study the extent and character of complex hydrocarbon seepage in the Bay of Campeche, southern Gulf of Mexico. Our observations showed that seafloor asphalt deposits previously only known from the Chapopote Knoll also occur at numerous other knolls and ridges in water depths from 1230 to 3150 m. In particular the deeper sites (Chapopopte and Mictlan knolls) were characterized by asphalt deposits accompanied by extrusion of liquid oil in form of whips or sheets, and in some places (Tsanyao Yang, Mictlan, and Chapopote knolls) by gas emission and the presence of gas hydrates in addition. Molecular and stable carbon isotopic compositions of gaseous hydrocarbons suggest their primarily thermogenic origin. Relatively fresh asphalt structures were settled by chemosynthetic communities including bacterial mats and vestimentiferan tube worms, whereas older flows appeared largely inert and devoid of corals and anemones at the deep sites. The gas hydrates at Tsanyao Yang and Mictlan Knolls were covered by a 5-to-10 cm-thick reaction zone composed of authigenic carbonates, detritus, and microbial mats, and were densely colonized by 1-2 m-long tube worms, bivalves, snails, and shrimps. This study increased knowledge on the occurrences and dimensions of asphalt fields and associated gas hydrates at the Campeche Knolls. The extent of all discovered seepage structure areas indicates that emission of complex hydrocarbons is a widespread, thus important feature of the southern Gulf of Mexico.
    Keywords: Area/locality; Center for Marine Environmental Sciences; Comment; Elevation of event; Event label; Gas bubble sampler; GBS; GeoB19318-9; GeoB19325-13; GeoB19336-15; GeoB19336-5; GeoB19336-8; GeoB19337-1; GeoB19337-12; GeoB19346-8; Gulf of Mexico; Latitude of event; Longitude of event; M114/2; M114/2_103-8; M114/2_75-9; M114/2_82-13; M114/2_93-15; M114/2_93-5; M114/2_93-8; M114/2_94-1; M114/2_94-12; MARUM; Meteor (1986); Methane/ethane ratio; Remote operated vehicle; ROV; Sample code/label; Site; δ13C, methane
    Type: Dataset
    Format: text/tab-separated-values, 48 data points
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  • 5
    Publication Date: 2024-01-15
    Keywords: Campaign of event; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DEPTH, water; Elevation of event; Event label; Gear; GeoB16805; GeoB16810; GeoB16814-1; GeoB16824; GeoB16828; GeoB16832; GeoB16836-1; GeoB16837-1; GeoB16838-1; GeoB16839-1; GeoB16840-1; GeoB16841-1; GeoB16842-1; GeoB16855-2; GeoB16860; GeoB20101-1; GeoB20105-1; GeoB20106-1; GeoB20107-1; GeoB20109-1; GeoB20110-1; GeoB20115-1; GeoB20121-1; GeoB20122-1; GeoB20123-1; GeoB20124-1; GeoB20131-1; GeoB20132-1; GeoB20133-1; GeoB20134-1; GeoB20201-1; GeoB20202-1; GeoB20203-1; GeoB20204-1; GeoB20205-1; GeoB20207-1; GeoB20208-1; GeoB20209-1; GeoB20210-1; GeoB20211-1; GeoB20213-1; GeoB20215-1; GeoB20216-1; GeoB20217-1; GeoB20218-1; GeoB20221-1; GeoB20223-1; GeoB20224-1; GeoB20225-1; GeoB20226-1; GeoB20227-1; GeoB20228-1; GeoB20229-1; GeoB20230-1; GeoB20231-1; GeoB20232-1; GeoB20233-1; GeoB20234-1; GeoB20235-1; GeoB20236-1; GeoB20237-1; GeoB20238-1; GeoB20239-1; GeoB20240-1; GeoB20241-1; GeoB20242-1; HE387; HE387/05-1; HE387/10-1; HE387/14-1; HE387/24-1; HE387/28-1; HE387/32-1; HE387/36-1; HE387/37-1; HE387/38-1; HE387/39-1; HE387/40-1; HE387/41-1; HE387/42-1; HE387/55-2; HE387/60-1; HE449; HE449/01-1; HE449/05-1; HE449/06-1; HE449/07-1; HE449/09-1; HE449/10-1; HE449/15-1; HE449/21-1; HE449/22-1; HE449/23-1; HE449/24-1; HE449/31-1; HE449/32-1; HE449/33-1; HE449/34-1; HE450; HE450/01-1; HE450/02-1; HE450/03-1; HE450/04-1; HE450/05-1; HE450/07-1; HE450/08-1; HE450/09-1; HE450/10-1; HE450/11-1; HE450/13-1; HE450/15-1; HE450/16-1; HE450/17-1; HE450/18-1; HE450/21-1; HE450/23-1; HE450/24-1; HE450/25-1; HE450/26-1; HE450/27-1; HE450/28-1; HE450/29-1; HE450/30-1; HE450/31-1; HE450/32-1; HE450/33-1; HE450/34-1; HE450/35-1; HE450/36-1; HE450/37-1; HE450/38-1; HE450/39-1; HE450/40-1; HE450/41-1; HE450/42-1; Heincke; Latitude of event; Longitude of event; MARUM; Methane; Methane, flux; North Greenland Sea; Optional event label; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 262 data points
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  • 6
    Publication Date: 2024-01-15
    Keywords: Campaign of event; Center for Marine Environmental Sciences; CTD/Rosette; CTD-RO; DEPTH, water; Elevation of event; Event label; Gear; GeoB16805; GeoB16810; GeoB16814-1; GeoB16824; GeoB16828; GeoB16832; GeoB16836-1; GeoB16837-1; GeoB16838-1; GeoB16839-1; GeoB16840-1; GeoB16841-1; GeoB16842-1; GeoB16843-1; GeoB16844-1; GeoB16855-2; GeoB20101-1; GeoB20105-1; GeoB20106-1; GeoB20107-1; GeoB20109-1; GeoB20110-1; GeoB20115-1; GeoB20121-1; GeoB20122-1; GeoB20123-1; GeoB20124-1; GeoB20131-1; GeoB20132-1; GeoB20133-1; GeoB20134-1; GeoB20201-1; GeoB20202-1; GeoB20203-1; GeoB20204-1; GeoB20205-1; GeoB20206-1; GeoB20207-1; GeoB20208-1; GeoB20209-1; GeoB20210-1; GeoB20211-1; GeoB20213-1; GeoB20215-1; GeoB20216-1; GeoB20217-1; GeoB20218-1; GeoB20221-1; GeoB20223-1; GeoB20224-1; GeoB20225-1; GeoB20226-1; GeoB20227-1; GeoB20228-1; GeoB20229-1; GeoB20230-1; GeoB20231-1; GeoB20232-1; GeoB20233-1; GeoB20234-1; GeoB20235-1; GeoB20236-1; GeoB20237-1; GeoB20238-1; GeoB20239-1; GeoB20240-1; GeoB20241-1; GeoB20242-1; HE387; HE387/05-1; HE387/10-1; HE387/14-1; HE387/24-1; HE387/28-1; HE387/32-1; HE387/36-1; HE387/37-1; HE387/38-1; HE387/39-1; HE387/40-1; HE387/41-1; HE387/42-1; HE387/43-1; HE387/44-1; HE387/55-2; HE449; HE449/01-1; HE449/05-1; HE449/06-1; HE449/07-1; HE449/09-1; HE449/10-1; HE449/15-1; HE449/21-1; HE449/22-1; HE449/23-1; HE449/24-1; HE449/31-1; HE449/32-1; HE449/33-1; HE449/34-1; HE450; HE450/01-1; HE450/02-1; HE450/03-1; HE450/04-1; HE450/05-1; HE450/06-1; HE450/07-1; HE450/08-1; HE450/09-1; HE450/10-1; HE450/11-1; HE450/13-1; HE450/15-1; HE450/16-1; HE450/17-1; HE450/18-1; HE450/21-1; HE450/23-1; HE450/24-1; HE450/25-1; HE450/26-1; HE450/27-1; HE450/28-1; HE450/29-1; HE450/30-1; HE450/31-1; HE450/32-1; HE450/33-1; HE450/34-1; HE450/35-1; HE450/36-1; HE450/37-1; HE450/38-1; HE450/39-1; HE450/40-1; HE450/41-1; HE450/42-1; Heincke; Latitude of event; Longitude of event; MARUM; Methane; Methane oxidation rate; North Greenland Sea; Optional event label; Turnover rate, methane oxidation; δ13C, methane
    Type: Dataset
    Format: text/tab-separated-values, 2284 data points
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  • 7
    facet.materialart.
    Unknown
    PANGAEA
    In:  MARUM - Center for Marine Environmental Sciences, University Bremen
    Publication Date: 2024-02-02
    Keywords: Center for Marine Environmental Sciences; Course; CT; DATE/TIME; DEPTH, water; Event label; Heading; LATITUDE; LONGITUDE; Maria S. Merian; MARUM; MSM57/1; MSM57/1-track; MSM57/2; MSM57/2-track; Position; Sound velocity in water; Speed; Temperature, water; Underway cruise track measurements; Wind direction; Wind direction, true; Wind speed; Wind speed, true
    Type: Dataset
    Format: text/tab-separated-values, 33506 data points
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  • 8
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Mau, Susan; Römer, Miriam; Torres, Marta E; Bussmann, Ingeborg; Pape, Thomas; Damm, Ellen; Geprägs, Patrizia; Wintersteller, Paul; Hsu, Chieh-Wei; Loher, Markus; Bohrmann, Gerhard (2017): Widespread methane seepage along the continental margin off Svalbard - from Bjørnøya to Kongsfjorden. Scientific Reports, 7, 42997, https://doi.org/10.1038/srep42997
    Publication Date: 2024-04-17
    Description: Numerous articles have recently reported on gas seepage offshore Svalbard, because the gas emission from these Arctic sediments was thought to result from gas hydrate dissociation, possibly triggered by anthropogenic ocean warming. We report on findings of a much broader seepage area, extending from 74° to 79°, where more than a thousand gas discharge sites were imaged as acoustic flares. The gas discharge occurs in water depths at and shallower than the upper edge of the gas hydrate stability zone and generates a dissolved methane plume that is hundreds of kilometer in length. Data collected in the summer of 2015 revealed that 0.02?7.7% of the dissolved methane was aerobically oxidized by microbes and a minor fraction (0.07%) was transferred to the atmosphere during periods of low wind speeds. Most flares were detected in the vicinity of the Hornsund Fracture Zone, leading us to postulate that the gas ascends along this fracture zone. The methane discharges on bathymetric highs characterized by sonic hard grounds, whereas glaciomarine and Holocene sediments in the troughs apparently limit seepage. The large scale seepage reported here is not caused by anthropogenic warming.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 9
  • 10
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