Impact of wind pattern and complex topography on snow microphysics during International Collaborative Experiment for PyeongChang 2018 Olympic and Paralympic winter games (ICE-POP 2018)

Kim, Kwonil; Bang, Wonbae; Chang, Eun-Chul; Tapiador, Francisco J.; Tsai, Chia-Lun; Jung, Eunsil; Lee, Gyuwon

doi:https://doi.org/10.5194/acp-21-11955-2021

Articles | Volume 21, issue 15

https://doi.org/10.5194/acp-21-11955-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Winter weather research in complex terrain during ICE-POP...

https://doi.org/10.5194/acp-21-11955-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 21, issue 15

Research article

|

10 Aug 2021

Research article |

| 10 Aug 2021

Impact of wind pattern and complex topography on snow microphysics during International Collaborative Experiment for PyeongChang 2018 Olympic and Paralympic winter games (ICE-POP 2018)

Kwonil Kim, Wonbae Bang, Eun-Chul Chang, Francisco J. Tapiador, Chia-Lun Tsai, Eunsil Jung, and Gyuwon Lee

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Final revised paper (published on 10 Aug 2021)
Preprint (discussion started on 12 Mar 2021)

Interactive discussion

Status: closed

RC1: 'Comment on acp-2021-128', Anonymous Referee #1, 13 Apr 2021

The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2021-128/acp-2021-128-RC1-supplement.pdf

Citation: https://doi.org/10.5194/acp-2021-128-RC1
RC2: 'Comment on acp-2021-128', Anonymous Referee #2, 12 May 2021

Title: Impact of wind pattern and complex topography on snow microphysics during ICE-POP 2018

The manuscript documents the microphysical characteristics of snow by analyzing the PARSIVEL and MRR data collected from ICE-POP 2017-2018. The snow events were classified by three different synoptic systems. The three type of synoptic systems are air-sea, cold low and warm low patterns. The results show distinct characteristics of snow. The aggregation process increases the size of the snow. The riming process has higher values of fall velocity of snow particle. Most of the conclusions are reasonable, but further detailed analysis is missing. However, the manuscript did a good job summarizing 20 snow events from ICE-POP 2017-2018.

Minor comments:

Line 55: “showed that the mean precipitation amount increased by about 45% in the presence of both Kaema high and low pressure. ” Any reference?

Line 419: “the size of the snow does not greatly enlarge.” Why? Evidence?

Line 422: Where is the second peak of reflectivity?

Citation: https://doi.org/10.5194/acp-2021-128-RC2
AC1: 'Reply to both reviewers', GyuWon Lee, 23 Jun 2021

The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2021-128/acp-2021-128-AC1-supplement.pdf

Citation: https://doi.org/10.5194/acp-2021-128-AC1

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by GyuWon Lee on behalf of the Authors (23 Jun 2021) Author's response Author's tracked changes Manuscript

ED: Referee Nomination & Report Request started (28 Jun 2021) by Timothy Garrett

RR by Anonymous Referee #1 (01 Jul 2021)

ED: Publish as is (06 Jul 2021) by Timothy Garrett

Short summary

This study analyzes the microphysical characteristics of snow in complex terrain and the nearby ocean according to topography and wind pattern during the ICE-POP 2018 campaign. The observations from collocated vertically pointing radars and disdrometers indicate that the riming in the mountainous region is likely caused by a strong shear and turbulence. The different behaviors of aggregation and riming were found by three different synoptic patterns (air–sea interaction, cold low, and warm low).