Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016

A model was developed for simulating the effects of airborne silver iodide (AgI) glaciogenic cloud seeding using the weather research and forecasting (WRF) model with a modified Morrison cloud microphysics scheme. This model was used to hindcast the weather conditions and effects of seeding for thre...

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Main Authors: Sanghee Chae, Ki-Ho Chang, Seongkyu Seo, Jin-Yim Jeong, Baek-Jo Kim, Chang Ki Kim, Seong Soo Yum, Jinwon Kim
Format: Article
Language:English
Published: Hindawi Limited 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/8453460
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spelling doaj-ca709641ddba4d3688a96ae617ba0ca72020-11-24T22:09:59ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/84534608453460Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016Sanghee Chae0Ki-Ho Chang1Seongkyu Seo2Jin-Yim Jeong3Baek-Jo Kim4Chang Ki Kim5Seong Soo Yum6Jinwon Kim7Applied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaApplied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaApplied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaApplied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaApplied Meteorology Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaNew and Renewable Energy Resource Center, Korea Institute of Energy Research, Daejeon 34129, Republic of KoreaDepartment of Atmospheric Sciences, Yonsei University, Seoul 03722, Republic of KoreaClimate Research Division, National Institute of Meteorological Sciences, Jeju 63568, Republic of KoreaA model was developed for simulating the effects of airborne silver iodide (AgI) glaciogenic cloud seeding using the weather research and forecasting (WRF) model with a modified Morrison cloud microphysics scheme. This model was used to hindcast the weather conditions and effects of seeding for three airborne seeding experiments conducted in 2016. The spatial patterns of the simulated precipitation and liquid water path (LWP) qualitatively agreed with the observations. Considering the observed wind fields during the seeding, the simulated spatiotemporal distributions of the seeding materials, AgI, and snowfall enhancements were found to be reasonable. In the enhanced snowfall cases, the process by which cloud water and vapor were converted into ice particles after seeding was also reasonable. It was also noted that the AgI residence time (>1 hr) above the optimum AgI concentration (105 m−3) and high LWP (>100 g m−2) were important factors for snowfall enhancements. In the first experiment, timing of the simulated snowfall enhancement agreed with the observations, which supports the notion that the seeding of AgI resulted in enhanced snowfall in the experiment. The model developed in this study will be useful for verifying the effects of cloud seeding on precipitation.http://dx.doi.org/10.1155/2018/8453460
collection DOAJ
language English
format Article
sources DOAJ
author Sanghee Chae
Ki-Ho Chang
Seongkyu Seo
Jin-Yim Jeong
Baek-Jo Kim
Chang Ki Kim
Seong Soo Yum
Jinwon Kim
spellingShingle Sanghee Chae
Ki-Ho Chang
Seongkyu Seo
Jin-Yim Jeong
Baek-Jo Kim
Chang Ki Kim
Seong Soo Yum
Jinwon Kim
Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
Advances in Meteorology
author_facet Sanghee Chae
Ki-Ho Chang
Seongkyu Seo
Jin-Yim Jeong
Baek-Jo Kim
Chang Ki Kim
Seong Soo Yum
Jinwon Kim
author_sort Sanghee Chae
title Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
title_short Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
title_full Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
title_fullStr Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
title_full_unstemmed Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016
title_sort numerical simulations of airborne glaciogenic cloud seeding using the wrf model with the modified morrison scheme over the pyeongchang region in the winter of 2016
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2018-01-01
description A model was developed for simulating the effects of airborne silver iodide (AgI) glaciogenic cloud seeding using the weather research and forecasting (WRF) model with a modified Morrison cloud microphysics scheme. This model was used to hindcast the weather conditions and effects of seeding for three airborne seeding experiments conducted in 2016. The spatial patterns of the simulated precipitation and liquid water path (LWP) qualitatively agreed with the observations. Considering the observed wind fields during the seeding, the simulated spatiotemporal distributions of the seeding materials, AgI, and snowfall enhancements were found to be reasonable. In the enhanced snowfall cases, the process by which cloud water and vapor were converted into ice particles after seeding was also reasonable. It was also noted that the AgI residence time (>1 hr) above the optimum AgI concentration (105 m−3) and high LWP (>100 g m−2) were important factors for snowfall enhancements. In the first experiment, timing of the simulated snowfall enhancement agreed with the observations, which supports the notion that the seeding of AgI resulted in enhanced snowfall in the experiment. The model developed in this study will be useful for verifying the effects of cloud seeding on precipitation.
url http://dx.doi.org/10.1155/2018/8453460
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