High-Resolution COSMO-CLM Modeling and an Assessment of Mesoscale Features Caused by Coastal Parameters at Near-Shore Arctic Zones (Kara Sea)

Abstract

Coastal Arctic regions are characterized by severe mesoscale weather events that include extreme wind speeds, and the rugged shore conditions, islands, and mountain ranges contribute to mesoscale event formation. High-resolution atmospheric modeling is a suitable tool to reproduce and estimate some of these events, and so the regional non-hydrostatic climate atmospheric model COSMO-CLM (Consortium for Small-scale Modeling developed within the framework of the international science group CLM-Community) was used to reproduce mesoscale circulation in the Arctic coast zone under various surface conditions. Mid-term experiments were run over the Arctic domain, especially over the Kara Sea region, using the downscaling approach, with ≈12 km and ≈3 km horizontal grid sizes. The best model configuration was determined using standard verification methods; however, the model run verification process raised questions over its quality and aptness based on the high level of small-scale coastline diversity and associated relief properties. Modeling case studies for high wind speeds were used to study hydrodynamic mesoscale circulation reproduction, and we found that although the model could not describe the associated wind dynamic features at all scales using ≈3 km resolution, it could simulate different scales of island wind shadow effects, tip jets, downslope winds, vortex chains, and so on, quite realistically. This initial success indicated that further research could reveal more about the detailed properties of mesoscale circulations and extreme winds by applying finer resolution modeling.

A Three-Year Climatology of the Wind Field Structure at Cape Baranova (Severnaya Zemlya, Siberia) from SODAR Observations and High-Resolution Regional Climate Model Simulations during YOPP

“…These differences were larger than the results of other verification studies for the CCLM [6,25,26,29,31]. A comparison of the CCLM with resolutions of 3 and 13 km with coastal stations in the Kara Sea for four months yielded mean wind biases in the range of ±0.5 m/s [32], but they also reported large errors for a station affected by strong downslope winds. Ref.…”

Convection‐permitting modeling with regional climate models: Latest developments and next steps

“…For more than a decade, CPRCMs have been used to simulate regional surface wind over complex terrain (Jiménez et al, 2010), offshore (Jiménez et al, 2015), and during storms (Schaaf & Feser, 2018; Platonov & Kislov, 2020) and polar lows (Revokatova et al, 2021). CPRCMs were deemed quite useful to identify regions with high wind energy potential (Carvalho et al, 2012) and where observational coverage could be improved (Jiménez et al, 2010).…”

Observations and Simulations of Meteorological Conditions over Arctic Thick Sea Ice in Late Winter during the Transarktika 2019 Expedition

“…CCLM has been used for several studies of polynyas (e.g., [13,24,25]). Verification studies for CCLM have been performed, e.g., using standard weather station data [4,26], radiosondes [27] and aircraft data [28]. For the present paper, CCLM is used with a horizontal resolution of 5 km for the Barents and Kara Sea (Figure 1).…”