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  • 1
    Online Resource
    Online Resource
    American Meteorological Society ; 2020
    In:  Journal of Climate Vol. 33, No. 7 ( 2020-04-01), p. 2681-2700
    In: Journal of Climate, American Meteorological Society, Vol. 33, No. 7 ( 2020-04-01), p. 2681-2700
    Abstract: The response of the European climate to the Atlantic multidecadal variability (AMV) remains difficult to isolate in observations because of the presence of strong internal variability and anthropogenically forced signals. Using model sensitivity experiments proposed within the CMIP6/Decadal Climate Prediction Project Component C (DCPP-C) framework, the wintertime AMV–Europe teleconnection is here investigated in large ensembles of pacemaker-type simulations conducted with the CNRM-CM5 global circulation model. To evaluate the sensitivity of the model response to the AMV amplitude, twin experiments with the AMV forcing pattern multiplied by 2 and 3 (2xAMV and 3xAMV, respectively) are performed in complement to the reference ensemble (1xAMV). Based on a flow analog method, we show that the AMV-forced atmospheric circulation tends to cool down the European continent, whereas the residual signal, mostly including thermodynamical processes, contributes to warming. In 1xAMV, both terms cancel each other, explaining the overall weak AMV-forced atmospheric signal. In 2xAMV and 3xAMV, the thermodynamical contribution overcomes the dynamical cooling and is responsible for milder and wetter conditions found at large scale over Europe. The thermodynamical term includes the advection of warmer and more humid oceanic air penetrating inland and the modification of surface radiative fluxes linked to both altered cloudiness and snow-cover reduction acting as a positive feedback with the AMV amplitude. The dynamical anomalous circulation combines 1) a remote response to enhanced diabatic heating acting as a Rossby wave source in the western tropical Atlantic and 2) a local response associated with warmer SST over the subpolar gyre favoring an anomalous high. The extratropical influence is reinforced by polar amplification due to sea ice melting in all the subarctic seas. The weight between the tropical–extratropical processes and associated feedbacks is speculated to partly explain the nonlinear sensibility of the response to the AMV forcing amplitude, challenging thus the use of the so-called pattern-scaling technique to evaluate teleconnectivity and related impacts associated with decadal variability.
    Type of Medium: Online Resource
    ISSN: 0894-8755 , 1520-0442
    RVK:
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2020
    detail.hit.zdb_id: 246750-1
    detail.hit.zdb_id: 2021723-7
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  • 2
    Online Resource
    Online Resource
    World Health Organization Regional Office for the Eastern Mediterranean (WHO/EMRO) ; 2018
    In:  Eastern Mediterranean Health Journal Vol. 24, No. 09 ( 2018-09-01), p. 823-829
    In: Eastern Mediterranean Health Journal, World Health Organization Regional Office for the Eastern Mediterranean (WHO/EMRO), Vol. 24, No. 09 ( 2018-09-01), p. 823-829
    Type of Medium: Online Resource
    ISSN: 1020-3397 , 1687-1634
    Language: Unknown
    Publisher: World Health Organization Regional Office for the Eastern Mediterranean (WHO/EMRO)
    Publication Date: 2018
    detail.hit.zdb_id: 2097065-1
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  • 3
    Online Resource
    Online Resource
    Elsevier BV ; 1996
    In:  Thermochimica Acta Vol. 275, No. 1 ( 1996-4), p. 83-91
    In: Thermochimica Acta, Elsevier BV, Vol. 275, No. 1 ( 1996-4), p. 83-91
    Type of Medium: Online Resource
    ISSN: 0040-6031
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1996
    detail.hit.zdb_id: 1500974-9
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  • 4
    Online Resource
    Online Resource
    Wiley ; 2010
    In:  ChemInform Vol. 27, No. 33 ( 2010-08-05), p. no-no
    In: ChemInform, Wiley, Vol. 27, No. 33 ( 2010-08-05), p. no-no
    Type of Medium: Online Resource
    ISSN: 0931-7597
    Language: English
    Publisher: Wiley
    Publication Date: 2010
    detail.hit.zdb_id: 2110203-X
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  • 5
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 1994
    In:  Journal of thermal analysis Vol. 42, No. 6 ( 1994-12), p. 1313-1318
    In: Journal of thermal analysis, Springer Science and Business Media LLC, Vol. 42, No. 6 ( 1994-12), p. 1313-1318
    Type of Medium: Online Resource
    ISSN: 0022-5215 , 1572-8943
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 1994
    detail.hit.zdb_id: 2017304-0
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  • 6
    Online Resource
    Online Resource
    American Association for the Advancement of Science (AAAS) ; 2021
    In:  Science Advances Vol. 7, No. 4 ( 2021-01-22)
    In: Science Advances, American Association for the Advancement of Science (AAAS), Vol. 7, No. 4 ( 2021-01-22)
    Abstract: Many studies have sought to constrain climate projections based on recent observations. Until recently, these constraints had limited impact, and projected warming ranges were driven primarily by model outputs. Here, we use the newest climate model ensemble, improved observations, and a new statistical method to narrow uncertainty on estimates of past and future human-induced warming. Cross-validation suggests that our method produces robust results and is not overconfident. We derive consistent observationally constrained estimates of attributable warming to date and warming rate, the response to a range of future scenarios, and metrics of climate sensitivity. We find that historical observations narrow uncertainty on projected future warming by about 50%. Our results suggest that using an unconstrained multimodel ensemble is no longer the best choice for global mean temperature projections and that the lower end of previous estimates of 21st century warming can now be excluded.
    Type of Medium: Online Resource
    ISSN: 2375-2548
    Language: English
    Publisher: American Association for the Advancement of Science (AAAS)
    Publication Date: 2021
    detail.hit.zdb_id: 2810933-8
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  • 7
    Online Resource
    Online Resource
    Copernicus GmbH ; 2022
    In:  Earth System Dynamics Vol. 13, No. 4 ( 2022-10-04), p. 1397-1415
    In: Earth System Dynamics, Copernicus GmbH, Vol. 13, No. 4 ( 2022-10-04), p. 1397-1415
    Abstract: Abstract. Building on CMIP6 climate simulations, updated global and regional observations, and recently introduced statistical methods, we provide an updated assessment of past and future warming over France. Following the IPCC AR6 and recent global-scale studies, we combine model results with observations to constrain climate change at the regional scale. Over mainland France, the forced warming in 2020 with respect to 1900–1930 is assessed to be 1.66 [1.41 to 1.90] ∘C, i.e., in the upper range of the CMIP6 estimates, and is almost entirely human-induced. A refined view of the seasonality of this past warming is provided through updated daily climate normals. Projected warming in response to an intermediate emission scenario is assessed to be 3.8 ∘C (2.9 to 4.8 ∘C) in 2100 and rises up to 6.7 [5.2 to 8.2] ∘C in a very high emission scenario, i.e., substantially higher than in previous ensembles of global and regional simulations. Winter warming and summer warming are expected to be about 15 % lower than and 30 % higher than the annual mean warming, respectively, for all scenarios and time periods. This work highlights the importance of combining various lines of evidence, including model and observed data, to deliver the most reliable climate information. This refined regional assessment can feed adaptation planning for a range of activities and provides additional rationale for urgent climate action. Code is made available to facilitate replication over other areas or political entities.
    Type of Medium: Online Resource
    ISSN: 2190-4987
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2022
    detail.hit.zdb_id: 2578793-7
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  • 8
    Online Resource
    Online Resource
    CAIRN ; 2022
    In:  Pour la Science Vol. N° 542 – Décembre, No. 12 ( 2022-11-29), p. 7-7
    In: Pour la Science, CAIRN, Vol. N° 542 – Décembre, No. 12 ( 2022-11-29), p. 7-7
    Type of Medium: Online Resource
    ISSN: 0153-4092
    Language: French
    Publisher: CAIRN
    Publication Date: 2022
    SSG: 11
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  • 9
    Online Resource
    Online Resource
    Copernicus GmbH ; 2023
    In:  Earth System Dynamics Vol. 14, No. 3 ( 2023-06-20), p. 685-695
    In: Earth System Dynamics, Copernicus GmbH, Vol. 14, No. 3 ( 2023-06-20), p. 685-695
    Abstract: Abstract. Most of the North Atlantic ocean has warmed over the last decades, except a region located over the subpolar gyre, known as the North Atlantic “warming hole” (WH), where sea surface temperature (SST) has in contrast decreased. Previous assessments have attributed part of this cooling to the anthropogenic forcings (ANT) – aerosols (AER) and greenhouse gases (GHGs) – modulated by decadal internal variability. Here, I use an innovative and proven statistical method which combines climate models and observations to confirm the anthropogenic role in the cooling of the warming hole. The impact of the aerosols is an increase in SST which is opposed to the effect of GHGs. The latter largely contribute to the cooling of the warming hole over the historical period. Yet, large uncertainties remain in the quantification of the impact of each anthropogenic forcing. The statistical method is able to reduce the model uncertainty in SST over the warming hole, both over the historical and future periods with a decrease of 65 % in the short term and up to 50 % in the long term. A model evaluation validates the reliability of the obtained projections. In particular, the projections associated with a strong temperature increase over the warming hole are now excluded from the likely range obtained after applying the method.
    Type of Medium: Online Resource
    ISSN: 2190-4987
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2023
    detail.hit.zdb_id: 2578793-7
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  • 10
    In: Journal of Climate, American Meteorological Society, Vol. 33, No. 20 ( 2020-10-15), p. 8671-8692
    Abstract: Political decisions, adaptation planning, and impact assessments need reliable estimates of future climate change and related uncertainties. To provide these estimates, different approaches to constrain, filter, or weight climate model projections into probabilistic distributions have been proposed. However, an assessment of multiple such methods to, for example, expose cases of agreement or disagreement, is often hindered by a lack of coordination, with methods focusing on a variety of variables, time periods, regions, or model pools. Here, a consistent framework is developed to allow a quantitative comparison of eight different methods; focus is given to summer temperature and precipitation change in three spatial regimes in Europe in 2041–60 relative to 1995–2014. The analysis draws on projections from several large ensembles, the CMIP5 multimodel ensemble, and perturbed physics ensembles, all using the high-emission scenario RCP8.5. The methods’ key features are summarized, assumptions are discussed, and resulting constrained distributions are presented. Method agreement is found to be dependent on the investigated region but is generally higher for median changes than for the uncertainty ranges. This study, therefore, highlights the importance of providing clear context about how different methods affect the assessed uncertainty—in particular, the upper and lower percentiles that are of interest to risk-averse stakeholders. The comparison also exposes cases in which diverse lines of evidence lead to diverging constraints; additional work is needed to understand how the underlying differences between methods lead to such disagreements and to provide clear guidance to users.
    Type of Medium: Online Resource
    ISSN: 0894-8755 , 1520-0442
    RVK:
    Language: Unknown
    Publisher: American Meteorological Society
    Publication Date: 2020
    detail.hit.zdb_id: 246750-1
    detail.hit.zdb_id: 2021723-7
    Location Call Number Limitation Availability
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