Links Built Sample Clauses

Links Built. Links with other work packages The coupled Stream1 simulations are the heart of PRIMAVERA, and are linked with almost all other work packages, most importantly  The (coupled and atmosphere-only) Stream1 simulations provide the basis to assess the benefits of increased model resolution within WP2.  The coupled Stream1 simulations provide reference simulations to assess the impact of new parameterizations developed within WP3 and applied in the coupled Stream2 simulations.  The high-resolution coupled Stream1 simulations also provide reference simulations to assess the benefits of even higher model resolution attempted within WP4.  Model climatology and initial conditions needed for the sensitivity experiments performed within WP5 are taken from the 1950-control simulations. Links with other projects / endusers  The coupled Stream1 simulations will, as CMIP6 HighResMIP simulations, be made publicly available on the ESGF data nodes, providing the basis for publications which will enter the IPCC AR6 report.  Scientists within the CLIVAR project working closely with PRIMAVERA scientists have shown interest in analysing the coupled Stream1 simulations. Their ideas have been presented at the PRIMAVERA General Assembly in November 2017.
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Links Built. The simulations performed as part of stream 2 will increase the contribution of PRIMAVERA to HighResMIP.
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Links Built. The analyses presented in this report are largely based on a wide range of sensitivity experiments performed within the WP3 (improved physical parameterizations; sections 3.2- 3.5) and WP4 (stochastic physics, section 3.6) groups. As such, the inferred outcomes of D2.3 analyses are complementary to the evaluations presented in D2.1 and D2.2 (assessing the impact of ocean and atmospheric model resolution, based on Stream 1 results), and contribute to create a strong linkage across WP2, WP3 and WP4.
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Links Built. WP3a scientists have worked with WP6 to implement EasyAerosol in HadGEM3. In return, WP6 contributed the additional EasyAerosol simulations analysed in Sections 3.1 and 3.4.
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Links Built. The achievement of the atmosphere-only stream 2 simulations will contribute to the completion of PRIMAVERA deliverables dealing with future projections (in particular D5.4). It will also contribute to the multi-model analysis that will be performed for the whole of HighResMIP. T xxxxx: Table 1: Status of PRIMAVERA Stream 2 – highresSST-future simulations. D6.6 : PRIMAVERA Stream 2 - highresSST-future Model name PRIMAVERA Partner number of additional members planned Length of each member (years) Period Covered member runs completed members cmorized members available on DMT (mark with an asterix members completed) Remarks AWI-CM-1-1-LR AWI 0 AWI-CM-1-1-HR AWI 0 CMCC-CM2-HR4 CMCC 0 CMCC-CM2-VHR4 CMCC 0 r2i1p1f2, r3i1p1f2, r4i1p1f2, r5i1p1f2, r6i1p1f2, r7i1p1f2, r2i1p1f2, r3i1p1f2, r4i1p1f2, r5i1p1f2, r6i1p1f2, r7i1p1f2, CNRM-CM6-1 CERFACS 9 36 2015-2050 r8i1p1f2, r9i1p1f2, r10i1p1f2 r8i1p1f2, r9i1p1f2, r10i1p1f2 will be directly published on ESGF@CNRM datanode in next weeks r2i1p1f2, r3i1p1f2, r4i1p1f2, r2i1p1f2, r3i1p1f2, r4i1p1f2, CNRM-CM6-1-HR CERFACS 9 00 0000-0000 r5i1p1f2, r6i1p1f2, r7i1p1f2, r8i1p1f2, r9i1p1f2, r10i1p1f2 r5i1p1f2, r6i1p1f2, r7i1p1f2, r8i1p1f2, r9i1p1f2, r10i1p1f2 will be directly published on ESGF@CNRM datanode in next weeks EC-Earth3P 2 36 r3i1p1f1 r3i1p1f1* EC-Earth3P-HR 2 36 r2i1p1f1, r3i1p1f1 r2i1p1f1, r3i1p1f1* ECMWF-IFS-LR ECMWF 0 ECMWF-IFS-MR ECMWF 0 ECMWF-IFS-HR ECMWF 0 r1i2p1f1, r1i3p1f1, r1i14p1f1, HadGEM3-GC31-LM MOHC 4 36 r1i15p1f1 r1i2p1f1, r1i3p1f1 r1i2p1f1*, r1i3p1f1* HadGEM3-GC31-MM MOHC 2 36 r1i2p1f1, r1i3p1f1 r1i2p1f1, r1i3p1f1 r1i2p1f1*, r1i3p1f1* HadGEM3-GC31-HM MOHC 2 36 r1i2p1f1, r1i3p1f1 r1i2p1f1, r1i3p1f1 r1i2p1f1*, r1i3p1f1* MPI-ESM1-2-HR MPI 0 MPI-ESM1-2-XR MPI 0 F igures:
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Links Built. This deliverable was supported by participants from WP10, who provided the project results presented in the DV and additional information. Additionally, we collaborated with other project partners, from different WPs, including WP9, to obtain data and indices. References Xxxxx, D. A. (2011). A colour scheme for the display of astronomical intensity images. arXiv preprint arXiv:1108.5083. Xxxxxxx, X., and Xxxxxx, X. (1990). Heuristic evaluation of user interfaces, Proc. ACM CHI'90 Conf. (Seattle, WA, 1-5 April), 249-256. Xxxxxxx, X. (1994). Heuristic evaluation. In Nielsen, X., and Xxxx, X.X. (Eds.), Usability Inspection Methods. Xxxx Xxxxx & Sons, New York, NY. Annex 1 The interview guide Purpose of this document This document lists out the tasks and topics that will be covered during the research sessions with scientists, researchers and different users of the Primavera Data Viewer taking place at BSC on November 2019. This document is a rough guide towards the points that will be covered and the order in which they will be discussed. It is not verbatim script so that the moderator may have a more natural conversation with participants and may explore points of interest, both expected and unexpected, as they arise. Overall research parameters Pre evaluation interview 1 Introduction Thanks so much for coming! You will be helping me to evaluate the Primavera Data Viewer in its current state. We are going to talk about different aspects of the processes you go through when analysing and looking for content in the Primavera Data Viewer. At certain points in our discussion I’m going to ask you to complete some tasks using the current platform. Our objective is to get a clear view of how you use the tool, in which kind of situations and how to improve the tool to meet your needs. To get the best results, I’d like to ask you to use a technique called 'think out loud'. This means I’d like you to tell me what you are thinking, feeling and doing whenever you are completing a task. It may feel a bit unnatural at first, but it gets easier as you go ahead. If you feel uncomfortable at any stage, just let me know and we can stop the session. I’m not evaluating you; I’m evaluating the tool, so there are no wrong answers. Please be as honest as you can, and don’t worry if you get stuck - it just means you’ve found a problem with the tool, which will help us to make it better. I'll be recording the session using software records audio and video, as well as what you do in ...
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Links Built. The achievement of the atmosphere-only stream 2 simulations will contribute to the completion of PRIMAVERA deliverables dealing with future projections (in particular D5.4). It will also contribute to the multi-model analysis that will be performed for the whole of HighResMIP.
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Links Built. There is a strong link with the CMIP6 DCPP activities meaning that in the end the PRIMAVERA results will be analysed by a much larger community, that of CMIP6. In particular, the presence of both low and high resolution simulations will certainly generate a wide interest beyond the PRIMAVERA teams. References: Xxxx, X. X., Xxxxx, X. X., Xxxxxx, C., Xxxxxx-Xxxxx, F., Xxxxxxxxxxx, X., Xxxxxxx, B., Xxxxxxx, X., Xxxxxx, M., Xxxxx, G. A., Xxxxxx, X., Xxxxxxx, W. A., Xxxxxx, X., and Xxxxxx, F.: The Decadal Climate Prediction Project, Geosci. Model Dev. Discuss., doi:10.5194/gmd- 2016-78, in review, 2016 (xxxx://xxx.xxxxxx-xxxxx-xxx-xxxxxxx.xxx/gmd-2016-78/ ) Xxxxxxxxx, Xxxxxxx; Xxxxxxx, Xxxx X, 2016a. The Transient and Equilibrium Climate Response to Rapid Summertime Sea Ice Loss in CCSM4. Journal of Climate Volume: 29 Issue: 2 Pages: 401-417 Xxxxxxxxx, R. and X. X. Xxxxxxx, 2016b. Isolating the atmospheric circulation response to Arctic sea-ice loss in the coupled climate system. Submitted to J. Climate, April 2016. (available on Xxxx Xxxxxxx website) Xxxxxx, X., Xxxxxx, X., Xxxxxxx-Xxxxxx, X., 2016a: Definition of the anomalous sea surface temperature patterns. Technical notes for DCPP-C experiments Xxxxxx, X., Xxxxxx, R., Xxxxxxx-Xxxxxx, Y., 2016b: Recommendations for ocean restoring and ensemble generation. Technical notes for DCPP-C experiments Xxxxx, X., X. Xxx, X. X. Xxxxx and J. Screen, 2016: Does ocean-coupling matter for the northern extra-tropical response to projected Arctic sea ice loss?Geophys. Res. Lett., doi: 10.1002/2016GL067792. Xxxxx, X., X. Xxxxxxx-Xxxxx, X. Xxxxxxx, X. Xxxxxxxx, X. Xxxxxx and X. Xxxxxx, Respective effects of Arctic sea ice loss and GHGs increase on the Northern Hemisphere atmospheric circulation, in revision for Climate Dynamics Xxxxxxx-Xxxxxx, Y., X. Xxxxxxxxxx, X. Xxxxxx, X. Xxxxxx, X. Xxxxxxxx and X. Xxxxxxxxxxx, 2016, Assessing the climate impacts of the observed Atlantic multidecadal variability using the GFDL CM2.1 and NCAR CESM1 global coupled models, J. Climate, submitted
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