Journal
JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS
Volume 15, Issue 2, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2022MS003175
Keywords
secondary eyewall formation; eyewall replacement cycle; sensitivity to model resolutions; mechanism for SEF; ERC
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Depicting Secondary Eyewall Formation (SEF) and Eyewall Replacement Cycle (ERC) in a numerical model is important for tropical cyclone (TC) forecasting. The impact of horizontal and vertical resolutions on SEF/ERC is examined through numerical experiments. Results show that SEF/ERC is manifested when the horizontal grid spacing is 2-km or smaller, while no obvious SEF/ERC is observed with grid spacings of 6-km and 4-km.
Depicting Secondary Eyewall Formation (SEF) and Eyewall Replacement Cycle (ERC) in a numerical model is important for tropical cyclone (TC) forecasting. However, there is no consensus about what resolutions are appropriate to describe SEF/ERC within a full-physics mesoscale model. In this study, numerical experiments are conducted to examine the impact of the horizontal and vertical resolutions on SEF/ERC. The mesoscale model is configured through nesting to the horizontal grid spacings of 6, 4, 2, 1.33, 0.67-km, and with 27- and 54-levels on an f-plane in a quiescent environment. In addition, there are more levels below 1.5-km to better describe the TC boundary layer (TCBL). The simulations with 6 and 4-km grid spacings show no obvious SEF/ERC regardless of the number of vertical levels. When the horizontal grid spacings decrease to 2-km or smaller, the simulations manifest SEF/ERC. These results are supported by a few simulations with the ARW model using similar configurations. Furthermore, the spectra of kinetic energy and vertical velocity from various resolutions confirm that the grid spacings should be smaller than 4-km to resolve SEF/ERC. The impact of doubling vertical levels on the SEF/ERC is not as significant as doubling the horizontal resolutions. Finally, we discuss the coupling between the balanced/unbalanced flows (above/in the TCBL), and their effect on SEF. It is proposed that the coupled balanced/unbalanced processes that generate the quasi-steady cooling zone in the primary eyewall and two warming regions inside and beyond the cooling zone are essential for SEF.
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