the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The KNMI Large Ensemble Time Slice (KNMI-LENTIS)
Laura Muntjewerf
Richard Bintanja
Thomas Reerink
Karin Wiel
Abstract. Large-ensemble modelling has become an increasingly popular approach to study the mean climate and the climate system’s internal variability in response to external forcing. Here we present the KNMI Large ENsemble TIme Slice (KNMI-LENTIS): a new large ensemble data set produced with the re-turned version of the global climate model EC-Earth3. The ensemble consists of two distinct time slices of 10 year each: a present-day time slice and a +2 K warmer future time slice relative to present-day. The initial conditions for the ensemble members are generated with a combination of micro and macro perturbations. The 10-year length of a single time slice is assumed to be too short to show a significant forced climate change signal, and the ensemble size of 1600 years (160 x 10 years) is assumed to be sufficient to sample the full distribution of climate variability. The time-slice approach makes it possible to study extreme events on sub-annual timescales as well as events that span multiple years such as multi-year droughts and preconditioned compound events. KNMI-LENTIS is therefore uniquely suited to study internal variability and extreme events both at a given climate state and those resulting from forced changes due to external radiative forcing. A unique feature of this ensemble is the high temporal output frequency of the surface water balance and surface energy balance variables, which are stored in 3-hourly intervals, allowing for detailed studies into extreme events. The data set is particularly geared towards research in the land-atmosphere domain. EC-Earth3 has a considerable warm bias in the Southern Ocean and over Antarctica. Hence, users of KNMI-LENTIS are advised to make in-depth comparisons with observational or reanalysis data especially if their studies focus on ocean processes, on locations in the Southern Hemisphere or on teleconnections involving both hemispheres. In this paper, we will give some examples to demonstrate the added value of KNMI-LENTIS for extreme and compound event research and for climate-impact modelling.
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Laura Muntjewerf et al.
Status: open (until 30 Mar 2023)
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RC1: 'Comment on egusphere-2022-1378', Anonymous Referee #1, 24 Feb 2023
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This paper introduces the new time slice large ensemble from KNMI. It is well written, describes the experiments in details and presents some interesting applications. I recommend it is accepted with minor revision as detailed below.
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45 change e.g. to ‘for example’
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Reference issue line 64
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Line 60 Could reference introduction paper to the large ensemble special issue: https://esd.copernicus.org/articles/12/401/2021/ and/or single forcing large ensembles e.g.: https://www.cesm.ucar.edu/working-groups/climate/simulations/cesm1-single-forcing-le and https://open.canada.ca/data/en/dataset/aa7b6823-fd1e-49ff-a6fb-68076a4a477c
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Line 71 – this seems like a good assumption but can you test it? Perhaps look at 1300 vs 1600 and see how different they are. After reading the paper I see the authors do test this. Perhaps allude to it here on line 71
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76 be consistent – should be 5 years
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149 – have you checked that there is no trend?
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174 – could replace ‘means’ with ‘refers to’
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178 – could replace ‘like’ with ‘such as’
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3 E can you suggest the ensemble mean is removed for variables where trend is too large as in many other le studies
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Section 3.5 you could cite and discuss the following papers:
https://wires.onlinelibrary.wiley.com/doi/full/10.1002/wcc.563
https://link.springer.com/article/10.1007/s00382-015-2806-8
https://journals.ametsoc.org/view/journals/clim/36/2/JCLI-D-21-0176.1.xml
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262 can you make a stronger statement than 'seems to'
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589 ??? Are confusing
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4.1 I don't see a reference to fig a/b
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Fig 7 no reference to b after a
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Figure 10 define PV in the caption please
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Citation: https://doi.org/10.5194/egusphere-2022-1378-RC1
Laura Muntjewerf et al.
Laura Muntjewerf et al.
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