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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: iv,113 Seiten , Illustrationen, Diagramme, Karten
    Series Statement: Report / Center for Climate System Research 16
    Language: English
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  • 2
    Publication Date: 2023-12-09
    Keywords: Bottle, Niskin; Calculated after Luo et al. (2012); Date/Time of event; DEPTH, water; Event label; KH-06-2/01; KH-06-2/02; KH-06-2/03; KH-06-2/04; KH-06-2/05; KH-06-2/06; KN-242/01; KN-242/02; KN-242/03; KN-242/04; KN-242/05; KN-242/06; KT-06-21/01; KT-06-21/02; KT-06-21/03; KT-06-21/04; KT-06-21/05; KT-07-22/01a; KT-07-22/01b; KT-07-22/02; KT-07-22/03; KT-07-22/04; KT-07-22/05; Latitude of event; Longitude of event; MAREDAT_Diazotrophs_Collection; MR07-01/01; MR07-01/02; MR07-01/03; MR07-01/04; MR07-01/05; MR07-01/06; MR07-01/07; MR07-01/08; MR07-01/09; MR07-01/10; MR07-01/11; MR07-06/01; MR07-06/02; MR07-06/03; MR07-06/04; MR07-06/05; MR07-06/06; MR07-06/07; MR07-06/08; MR07-06/09; MR07-06/10; MR07-06/11; MR07-06/12; MR07-06/13; MR07-06/14; MR07-06/15; MR07-06/16; MR07-06/17; MR07-06/18; MR07-06/19; MR07-06/20; MR07-06/21; MR07-06/22; MR07-06/23; MR07-06/24; MR07-06/25; NIS; Nitrate; Nitrogen Fixation (C2H2 Reduction); Nitrogen fixation rate, total; Nitrogen fixation rate, whole seawater; Pacific; Phosphate; Salinity; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 618 data points
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  • 3
    Publication Date: 2024-04-15
    Description: The climate science community aims to improve our understanding of climate change due to anthropogenic influences on atmospheric composition and the Earth's surface. Yet not all climate interactions are fully understood and diversity in climate model experiments persists as assessed in the latest Intergovernmental Panel on Climate Change (IPCC) assessment report. This article synthesizes current challenges and emphasizes opportunities for advancing our understanding of climate change and model diversity. The perspective of this article is based on expert views from three multi-model intercomparison projects (MIPs) – the Precipitation Driver Response MIP (PDRMIP), the Aerosol and Chemistry MIP (AerChemMIP), and the Radiative Forcing MIP (RFMIP). While there are many shared interests and specialisms across the MIPs, they have their own scientific foci and specific approaches. The partial overlap between the MIPs proved useful for advancing the understanding of the perturbation-response paradigm through multi-model ensembles of Earth System Models of varying complexity. It specifically facilitated contributions to the research field through sharing knowledge on best practices for the design of model diagnostics and experimental strategies across MIP boundaries, e.g., for estimating effective radiative forcing. We discuss the challenges of gaining insights from highly complex models that have specific biases and provide guidance from our lessons learned. Promising ideas to overcome some long-standing challenges in the near future are kilometer-scale experiments to better simulate circulation-dependent processes where it is possible, and machine learning approaches for faster and better sub-grid scale parameterizations where they are needed. Both would improve our ability to adopt a smart experimental design with an optimal tradeoff between resolution, complexity and simulation length. Future experiments can be evaluated and improved with sophisticated methods that leverage multiple observational datasets, and thereby, help to advance the understanding of climate change and its impacts.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 4
    Publication Date: 2024-02-07
    Description: Feedbacks play a fundamental role in determining the magnitude of the response of the climate system to external forcing, such as from anthropogenic emissions. The latest generation of Earth system models includes aerosol and chemistry components that interact with each other and with the biosphere. These interactions introduce a complex web of feedbacks that is important to understand and quantify. This paper addresses multiple pathways for aerosol and chemical feedbacks in Earth system models. These focus on changes in natural emissions (dust, sea salt, dimethyl sulfide, biogenic volatile organic compounds (BVOCs) and lightning) and changes in reaction rates for methane and ozone chemistry. The feedback terms are then given by the sensitivity of a pathway to climate change multiplied by the radiative effect of the change. We find that the overall climate feedback through chemistry and aerosols is negative in the sixth Coupled Model Intercomparison Project (CMIP6) Earth system models due to increased negative forcing from aerosols in a climate with warmer surface temperatures following a quadrupling of CO2 concentrations. This is principally due to increased emissions of sea salt and BVOCs which are sensitive to climate change and cause strong negative radiative forcings. Increased chemical loss of ozone and methane also contributes to a negative feedback. However, overall methane lifetime is expected to increase in a warmer climate due to increased BVOCs. Increased emissions of methane from wetlands would also offset some of the negative feedbacks. The CMIP6 experimental design did not allow the methane lifetime or methane emission changes to affect climate, so we found a robust negative contribution from interactive aerosols and chemistry to climate sensitivity in CMIP6 Earth system models.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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