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  • 1
    Online Resource
    Online Resource
    Berlin, Heidelberg :Springer Berlin / Heidelberg,
    Keywords: Earth sciences. ; Geology. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (141 pages)
    Edition: 1st ed.
    ISBN: 9783642322358
    Series Statement: SpringerBriefs in Earth System Sciences Series
    Language: English
    Note: Intro -- Earth System Science: Bridging the Gaps between Disciplines -- Preface -- Acknowledgments -- Contents -- 1 Introduction -- 1.1…General Aspects of Earth System Science -- 1.2…The Structural and Educational Concept in an Interdisciplinary Research School for Earth System Science -- 1.2.1 The Supervision and Mentoring Concept -- 1.2.2 The Managing Concept -- 1.2.3 The Helmholtz Certificate -- 2 Remote Sensing and Modelling of Atmospheric Chemistry and Sea Ice Parameters -- 2.1…NO2 Pollution Trends Over Megacities 1996--2010 from Combined Multiple Satellite Data Sets -- 2.1.1 Introduction -- 2.1.2 Method -- 2.1.3 Results -- 2.1.4 Discussion and Conclusion -- 2.2…A Brief Example on the Application of Remotely Sensed Tracer Observations in Atmospheric Science---Studying the Impact of Stratosphere--Mesosphere Coupling on Polar Ozone Variability -- 2.2.1 Introduction -- 2.2.2 CO as Tracer in the Polar Stratosphere and Mesosphere -- 2.2.3 Measurements of CO by Microwave Radiometry -- 2.2.4 Interpretation of the KIMRA CO Time Series -- 2.2.5 Summary and Conclusion -- 2.3…Contamination of the Western Pacific Atmosphere -- 2.3.1 Introduction -- 2.3.2 Method -- 2.3.3 Results -- 2.3.4 Discussion and Conclusion -- 2.4…Three Dimensional Model Simulations of the Impact of Solar Proton Events on Nitrogen Compounds and Ozone in the Middle Atmosphere -- 2.4.1 Introduction -- 2.4.2 Model SimulationsModel Simulations -- 2.4.2.1 The B3dCTM -- 2.4.2.2 Model Simulations of SPEs -- 2.4.3 Model Simulation Results -- 2.4.4 Summary and Discussion -- 2.5…Evaluation of the Coupled and Extended SCIATRAN Version Including Radiation Processes Within the Water: Initial Results -- 2.6…Improving the PhytoDOAS Method to Retrieve Coccolithophores Using Hyper-Spectral Satellite Data -- 2.6.1 Introduction -- 2.6.1.1 Motivation -- 2.6.1.2 The Importance of Coccolithophores. , 2.6.1.3 Objectives -- 2.6.2 Material and Method -- 2.6.2.1 From DOAS to PhytoDOAS -- 2.6.2.2 Improvement to PhytoDOAS -- 2.6.2.3 Satellite and Modeled Data -- 2.6.3 Results and Discussion -- 2.6.3.1 Global Distribution of Coccolithophores -- 2.6.3.2 Time Series of Monitored Parameters in a Selected Region of the North Atlantic -- 2.6.4 Conclusions and Outlook -- 2.7…Primary Productivity and Circulation Patterns Downstream of South Georgia: A Southern Ocean Example of the ''Island Mass Effect'' -- 2.7.1 Introduction -- 2.7.2 Data and Methods -- 2.7.3 Results and Discussion -- 2.7.4 Conclusions -- 2.8…Summer Sea Ice Concentration Changes in the Weddell Sea and Their Causes -- 2.8.1 Introduction -- 2.8.2 Data -- 2.8.3 Results and Discussion -- 2.8.4 Conclusion -- 2.9…Validation of the Snow Grain Size Retrieval SGSP Using Six Ground Truth Data Sets -- 2.9.1 Introduction -- 2.9.2 The SGSP Retrieval -- 2.9.3 Validation Studies -- 2.9.4 Discussion and Conclusion -- References -- 3 Earth System Modelling and Data Analysis -- 3.1…The Last Interglacial as Simulated by an Atmosphere--Ocean General Circulation Model: Sensitivity Studies on the Influence of the Greenland Ice Sheet -- 3.1.1 Introduction -- 3.1.2 Model Description and Experimental Setup -- 3.1.2.1 Model Description -- 3.1.2.2 Experimental Setup -- 3.1.3 Results -- 3.1.4 Discussion and Conclusions -- 3.2…Simulated Caribbean Climate Variability During the Mid-Holocene -- 3.2.1 Introduction -- 3.2.2 Method -- 3.2.2.1 Model Description -- 3.2.2.2 Experiment Setup -- 3.2.3 Results -- 3.2.3.1 Mean Climatology -- 3.2.3.2 Climate Variability Associated with the ENSO -- 3.2.3.3 Climate Variability Associated with the AMO -- 3.2.4 Discussion and Conclusion -- 3.3…Oceanic delta 18O Variation and its Relation to Salinity in the MPI-OM Ocean Model -- 3.3.1 Introduction -- 3.3.2 Method -- 3.3.2.1 Ocean Model. , 3.3.2.2 Isotope Tracer H218O -- 3.3.2.3 Observation Database of delta 18O -- 3.3.3 Results -- 3.3.4 Discussion and Conclusion -- 3.4…Ocean Adjustment to High-Latitude Density Perturbations -- 3.4.1 Introduction -- 3.4.2 Model Set-up -- 3.4.3 Results -- 3.4.4 Discussion and Conclusion -- References -- 4 Geotectonics -- 4.1…Continental Deformation of Antarctica During Gondwana's Breakup -- 4.1.1 Introduction -- 4.1.2 Method and Data -- 4.1.3 Results -- 4.1.4 Discussion and Summary -- Acknowledgments -- References -- 5 Climate Archives -- 5.1…The Inorganic Carbon System in the Deep Southern Ocean and Glacial-Interglacial Atmospheric CO2 -- 5.1.1 Introduction -- 5.1.2 Objective/Study Area/Materials and Methods -- 5.1.3 Results/Discussion -- 5.1.4 Outlook -- 5.2…The Significance of the Long Lived ( greaterthan 400 Years) Bivalve Arctica Islandica as a High-Resolution Bioarchive -- 5.2.1 Introduction -- 5.2.2 Methods -- 5.2.2.1 Effect of Sample Preparation -- 5.2.2.2 Lead, Barium, and Manganese Measurements -- 5.2.3 Results and Discussion -- 5.2.3.1 Effect of Sample Preparation -- 5.2.3.2 Lead as a Pollution Tracer -- 5.2.3.3 Barium and Manganese as Indicators of Primary Production -- 5.2.4 Conclusion -- 5.3…Sub-Annual Resolution Measurements of Dust Concentration and Size in Different Time Slices of the NorthGRIP Ice Core -- 5.3.1 Introduction -- 5.3.2 Method -- 5.3.3 Results -- 5.3.4 Discussion and Conclusion -- Acknowledgments -- References -- 6 Ecosystems and Climate Change -- 6.1…Predicting Habitat Suitability for Cold-Water Coral Lophelia pertusa Using Multiscale Terrain Variables -- 6.1.1 Introduction -- 6.1.2 Materials and Method -- 6.1.2.1 Study Area -- 6.1.2.2 Multiscale Terrain Variables -- 6.1.2.3 Predictive Method: Maxent -- 6.1.3 Results -- 6.1.4 Discussion and Conclusion -- References -- 7 Geoinformatics. , 7.1…Resource-Aware Decomposition and Orchestration of Geoprocessing Requests in a SOA Framework -- 7.1.1 Introduction -- 7.1.2 Query Decomposition and Orchestration -- 7.1.3 Performance Evaluation -- 7.1.4 Conclusion -- 7.2…A Specification-Based Quality Model to Improve Confidence in Web Services of Multidisciplinary Earth System Science -- 7.2.1 Introduction -- 7.2.2 Methods -- 7.2.3 Results -- 7.2.4 Discussion and Conclusion -- References -- 8 Geoengineering -- 8.1…Feasibility Study of Using a Petroleum Systems Modeling Software to Evaluate Basin Scale Pressure Evolution Associated With CO2 Storage -- 8.1.1 Introduction -- 8.1.2 Principles of Petroleum Systems Modelling -- 8.1.3 CO2 Injection Method in PetroMod -- 8.1.4 Evaluation of the Pressure Buildup in PetroMod -- 8.1.4.1 Method -- 8.1.4.2 Results -- 8.1.5 Discussion and Conclusion -- Acknowledgments -- References.
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  • 2
    Online Resource
    Online Resource
    [s.l.] : Springer-Verlag
    Keywords: Electronic books
    Description / Table of Contents: This work provides a short 'getting started' guide to Fortran 90/95. The main target audience consists of newcomers to the field of numerical computation within Earth system sciences (students, researchers or scientific programmers). Furthermore, readers accustomed to other programming languages may also benefit from this work, by discovering how some programming techniques they are familiar with map to Fortran 95. The main goal is to enable readers to quickly start using Fortran 95 for writing useful programs. It also introduces a gradual discussion of Input/Output facilities relevant for Earth system sciences, from the simplest ones to the more advanced netCDF library (which has become a de facto standard for handling the massive datasets used within Earth system sciences). While related works already treat these disciplines separately (each often providing much more information than needed by the beginning practitioner), the reader finds in this book a shorter guide which links them. Compared to other books, this work provides a much more compact view of the language, while also placing the language-elements in a more applied setting, by providing examples related to numerical computing and more advanced Input/Output facilities for Earth system sciences. Naturally, the coverage of the programming language is relatively shallow, since many details are skipped. However, many of these details can be learned gradually by the practitioner, after getting an overview and some practice with the language through this book.
    Type of Medium: Online Resource
    Pages: Online Ressource (5414 KB, 250 S.)
    Edition: 1. Aufl.
    ISBN: 364237008X
    DDC: 005.13
    Language: English
    Note: Description based upon print version of record , Preface; Contents; Acronyms; 1 General Concepts; 1.1 History and Evolution of the Language; 1.2 Essential Toolkit (Compilers); 1.3 Basic Programming Workflow; References; 2 Fortran Basics; 2.1 Program Layout; 2.2 Keywords, Identifiers and Code Formatting; 2.3 Scalar Values and Constants; 2.3.1 Declarations for Scalars of Numeric Types; 2.3.2 Representation of Numbers and Limitations of Computer Arithmetic; 2.3.3 Working with Scalars of Numeric Types; 2.3.4 The [basicstyle=,keywordstyle=,identifierstyle=]kind type-parameter; 2.3.5 Some Numeric Intrinsic Functions , 2.3.6 Scalars of Non-numeric Types2.4 Input/Output (I/O); 2.4.1 List-Directed Formatted I/O to Screen/from Keyboard; 2.4.2 Customizing Format-Specifications; 2.4.3 Information Pathways: Customizing I/O Channels; 2.4.4 The Need for More Advanced I/O Facilities; 2.5 Program Flow-Control Elements ([basicstyle=,keywordstyle=,identifierstyle=]if, [basicstyle=,keywordstyle=,identifierstyle=]case, Loops, etc.); 2.5.1 [basicstyle=,keywordstyle=,identifierstyle=]if Construct; 2.5.2 [basicstyle=,keywordstyle=,identifierstyle=]case Construct , 2.5.3 [basicstyle=,keywordstyle=,identifierstyle=]do Construct2.6 Arrays and Array Notation; 2.6.1 Declaring Arrays; 2.6.2 Layout of Elements in Memory; 2.6.3 Selecting Array Elements; 2.6.4 Writing Data into Arrays; 2.6.5 I/O for Arrays; 2.6.6 Array Expressions; 2.6.7 Using Arrays for Flow-Control; 2.6.8 Memory Allocation and Dynamic Arrays; 2.7 More Intrinsic Procedures; 2.7.1 Acquiring Date and Time Information; 2.7.2 Random Number Generators (RNGs); References; 3 Elements of Software Engineering; 3.1 Motivation; 3.2 Structured Programming (SP) in Fortran
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  • 3
    Keywords: Climatic changes ; Climatic changes Simulation methods ; Climatic changes Forecasting ; Paleoclimatology ; Paleoclimatology Simulation methods ; Earth sciences Research ; Methodology ; System theory ; Interdisciplinary research ; Aufsatzsammlung ; Klima ; Geosphäre
    Description / Table of Contents: Earth system science is traditionally split into various disciplines (Geology, Physics, Meteorology, Oceanography, Biology etc.) and several sub-disciplines. Overall, the diversity of expertise provides a solid base for interdisciplinary research. However, gaining holistic insights into the Earth system requires the integration of observations, paleoclimate data, analysis tools and modeling. These different approaches of Earth system science are rooted in various disciplines that cut across a broad range of timescales. It is, therefore, necessary to link these disciplines at a relatively early stage in PhD programs. The linking of data and modeling, as it is the special emphasis in our graduate school, enables graduate students from a variety of disciplines to cooperate and exchange views on the common theme of Earth system science, which leads to a better understanding of processes within a global context
    Type of Medium: Book
    Pages: XI, 134 S. , Ill., graph. Darst., Kt. , 24 cm
    ISBN: 3642322344 , 9783642322341
    Series Statement: Springer briefs in earth system sciences
    DDC: 550.72
    RVK:
    Language: English
    Note: 1. Introduction-- 2. Remote Sensing and Modelling of Atmospheric Chemistry-- 3. Earth System Modelling and Data Analysis-- 4. Geotectonics-- 5. Climate Archives-- 6. Ecosystems and Climate Change-- 7. Geoinformatics-- 8. Geoengeneering. , General aspects of earth system science , The structural and educational concept in an interdisciplinary research school for earth system science , NO₂ pollution trends over megacities 1996-2010 from combined multiple satellite data sets , A brief example on the application of remotely sensed tracer observations in atmospheric science : studying the impact of stratosphere-mesosphere coupling on polar ozone variability , Contamination of the western Pacific atmosphere , Three dimensional model simulations of the impact of solar proton events on nitrogen compounds and ozone in the middle atmosphere , Evaluation of the coupled and extended SCIATRAN version including radiation processes within the water : initial results , Improving the PhytoDOAS method to retrieve coccolithophores using hyper-spectral satellite data , Primary productivity and circulation patterns downstream of South Georgia : a Southern Ocean "island mass effect" , Summer sea ice concentration changes in the Weddell Sea and their causes , Validation of the snow grain size retrieval SGSP using six ground truth data sets , The last interglacial as simulated by an atmosphere-ocean general circulation model : sensitivity studies on the influence of the Greenland ice sheet , Simulated Caribbean climate variability during the mid-Holocene , Oceanic [delta]¹⁸O variation and its relation to salinity in the MPI-OM ocean model , Ocean adjustment to high-latitude density perturbations , Continental deformation of Antarctica during Gondwana's breakup , The inorganic carbon system in the deep Southern Ocean and glacial-interglacial atmospheric CO₂ , The significance of the long lived (〉400 years) bivalve Arctica islandica as a high-resolution bioarchive , Sub-annual resolution measurements of dust concentration and size in different time slices of the NorthGRIP ice core , Predicting habitat suitability of cold-water coral Lophelia pertusa using multiscale terrain variables , Resource-aware decomposition and orchestration of geoprocessing requests in a SOA framework , A specification-based quality model to improve confidence in Web services of multidisciplinary earth system science , Feasibility study of using a petroleum systems modeling software to evaluate basin scale pressure evolution associated with CO₂ storage
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  • 4
    Keywords: Forschungsbericht ; Pazifischer Ozean Nord ; Paläoklima
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (50 Seiten, 11,20 MB) , Diagramme
    Language: German
    Note: Förderkennzeichen BMBF 03F0785A
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  • 5
    Online Resource
    Online Resource
    Bremerhaven : Alfred-Wegener-Institut (AWI) Helmholtz-Zentrum für Polar- und Meeresforschung
    Keywords: Forschungsbericht ; Pleistozän ; Paläoklima ; Modell ; Simulation ; Meer ; Kohlenstoffkreislauf
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (15 Seiten, 223,21 KB)
    Language: German , English
    Note: Förderkennzeichen BMBF 01LP1504A-D , Verbundnummer 01162215 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Literaturangaben , Sprache der Kurzfassungen: Deutsch, Englisch
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  • 6
    Publication Date: 2019-05-10
    Description: Proxy reconstructions of tropical Atlantic sea surface temperature (SST) that extend beyond the period of instrumental observations have primarily focused on centennial to millennial variability rather than on seasonal to multidecadal variability. Here we present monthly-resolved records of Sr/Ca (a proxy of SST) from fossil annually-banded Diploria strigosa corals from Bonaire (southern Caribbean Sea). The individual corals provide time-windows of up to 68 years length, and the total number of 295 years of record allows for assessing the natural range of seasonal to multidecadal SST variability in the western tropical Atlantic during snapshots of the mid- to late Holocene. Comparable to modern climate, the coral Sr/Ca records reveal that mid- to late Holocene SST was characterised by clear seasonal cycles, persistent quasi-biennial and prominent interannual as well as inter- to multidecadal-scale variability. However, the magnitude of SST variations on these timescales has varied over the last 6.2 ka. The coral records show increased seasonality during the mid-Holocene consistent with climate model simulations indicating that southern Caribbean SST seasonality is induced by insolation changes on orbital timescales, whereas internal dynamics of the climate system play an important role on shorter timescales. Interannual SST variability is linked to ocean–atmosphere interactions of Atlantic and Pacific origin. Pronounced interannual variability in the western tropical Atlantic is indicated by a 2.35 ka coral, possibly related to a strengthening of the variability of the El Niño/Southern Oscillation throughout the Holocene. Prominent inter- to multidecadal SST variability is evident in the coral records and slightly more pronounced in the mid-Holocene. We finally argue that our coral data provide a target for studying Holocene climate variability on seasonal and interannual to multidecadal timescales, when using further numerical models and high-resolution proxy data.
    Type: Article , PeerReviewed
    Format: text
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  • 7
    Publication Date: 2023-02-08
    Description: Rapid monsoon changes since the last deglaciation remain poorly constrained due to the scarcity of geological archives. Here we present a high-resolution scanning X-ray fluorescence (XRF) analysis of a 13.5 m terrace succession on the western Chinese Loess Plateau (CLP) to infer rapid monsoon changes since the last deglaciation. Our results indicate that Rb∕Sr and Zr∕Rb are sensitive indicators of chemical weathering and wind sorting, respectively, which are further linked to the strength of the East Asian summer monsoon (EASM) and the East Asian winter monsoon (EAWM). During the last deglaciation, two cold intervals of the Heinrich event 1 and Younger Dryas were characterized by intensified winter monsoon and weakened summer monsoon. The EAWM gradually weakened at the beginning of the Holocene, while the EASM remained steady till 9.9 ka and then grew stronger. Both the EASM and EAWM intensities were relatively weak during the Middle Holocene, indicating a mid-Holocene climatic optimum. Rb∕Sr and Zr∕Rb exhibit an antiphase relationship between the summer and winter monsoon changes on a centennial timescale during 16–1 ka. Comparison of these monsoon changes with solar activity and North Atlantic cooling events reveals that both factors can lead to abrupt changes on a centennial timescale in the Early Holocene. During the Late Holocene, North Atlantic cooling became the major forcing of centennial monsoon events.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2023-02-08
    Description: The past provides evidence of abrupt climate shifts and changes in the frequency of climate and weather extremes. We explore the non‐linear response to orbital forcing and then consider climate millennial variability down to daily weather events. Orbital changes are translated into regional responses in temperature, where the precessional response is related to nonlinearities and seasonal biases in the system. We question regularities found in climate events by analyzing the distribution of inter‐event waiting times. Periodicities of about 900 and 1150 years are found in ice cores besides the prominent 1500‐years cycle. However, the variability remains indistinguishable from a random process, suggesting that centennial‐to‐millennial variability is stochastic in nature. New numerical techniques are developed allowing for a high resolution in the dynamically relevant regions like coasts, major upwelling regions, and high latitudes. Using this model, we find a strong sensitivity of the Atlantic meridional overturning circulation depending on where the deglacial meltwater is injected into. Meltwater into the Mississippi and near Labrador hardly affect the large‐scale ocean circulation, whereas subpolar hosing mimicking icebergs yields a quasi shutdown. The same multi‐scale approach is applied to radiocarbon simulations enabling a dynamical interpretation of marine sediment cores. Finally, abrupt climate events also have counterparts in the recent climate records, revealing a close link between climate variability, the statistics of North Atlantic weather patterns, and extreme events.
    Type: Article , PeerReviewed
    Format: text
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  • 9
    Publication Date: 2023-02-08
    Description: A compilation of the published literature on dust content in terrestrial and marine sediment cores was synchronized with pollen data and speleothem growth phases on the Greenland Ice Core Chronology 2005 (GICC05) time axis. Aridity patterns for eight key areas of the global climate system have been reconstructed for the last 60 000 years. These records have different time resolutions and different dating methods, i.e. different types of stratigraphy. Nevertheless, all regions analysed in this study show humid conditions during early Marine Isotope Stage 3 (MIS3) and the early Holocene or deglaciation, but not always at the same time. Such discrepancies have been interpreted as regional effects, although stratigraphic uncertainties may affect some of the proposed interpretations. In comparison, most of the MIS2 interval becomes arid in all of the Northern Hemisphere records, but the peak arid conditions of the Last Glacial Maximum (LGM) and Heinrich event 1 differ in duration and intensity among regions. In addition, we also compare the aridity synthesis with modelling results using a global climate model (GCM). Indeed, geological archives and GCMs show agreement on the aridity pattern for the Holocene or deglaciation, for the LGM and for late MIS3.
    Type: Article , PeerReviewed
    Format: text
    Format: archive
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  • 10
    Publication Date: 2023-02-08
    Description: The earliest part of the Holocene, from 11.5k to 7k (k = 1000 years before present), is a critical transition period between the relatively cold last deglaciation and the warm middle Holocene. It is marked by more pronounced seasonality and reduced greenhouse gases (GHGs) than the present state, as well as by the presence of the Laurentide Ice Sheet (LIS) and glacial meltwater perturbation. This paper performs experiments under pre-industrial and different early-Holocene regimes with AWI-ESM (Alfred Wegener Institute–Earth System Model), a state-of-the-art climate model with unstructured mesh and varying resolutions, to examine the sensitivity of the simulated Atlantic meridional overturning circulation (AMOC) to early-Holocene insolation, GHGs, topography (including properties of the ice sheet), and glacial meltwater perturbation. In the experiments with early-Holocene Earth orbital parameters and GHGs applied, the AWI-ESM simulation shows a JJA (June–July–August) warming and DJF (December–January–February) cooling over the mid and high latitudes compared with pre-industrial conditions, with amplification over the continents. The presence of the LIS leads to an additional regional cooling over the North America. We also simulate the meltwater event around 8.2k. Big discrepancies are found in the oceanic responses to different locations and magnitudes of freshwater discharge. Our experiments, which compare the effects of freshwater release evenly across the Labrador Sea to a more precise injection along the western boundary of the North Atlantic (the coastal region of LIS), show significant differences in the ocean circulation response, as the former produces a major decline of the AMOC and the latter yields no obvious effect on the strength of the thermohaline circulation. Furthermore, proglacial drainage of Lakes Agassiz and Ojibway leads to a fast spin-down of the AMOC, followed, however, by a gradual recovery. Most hosing experiments lead to a warming over the Nordic Sea and Barents Sea of varying magnitudes, because of an enhanced inflow from lower latitudes and a northward displacement of the North Atlantic deep convection. These processes exist in both of our high- and low-resolution experiments, but with some local discrepancies such as (1) the hosing-induced subpolar warming is much less pronounced in the high-resolution simulations; (2) LIS coastal melting in the high-resolution model leads to a slight decrease in the AMOC; and (3) the convection formation site in the low- and high-resolution experiments differs, in the former mainly over northeastern North Atlantic Ocean, but in the latter over a very shallow subpolar region along the northern edge of the North Atlantic Ocean. In conclusion, we find that our simulations capture spatially heterogeneous responses of the early-Holocene climate.
    Type: Article , PeerReviewed
    Format: text
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