2020
DOI: 10.1029/2019jd031312
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The Role of Ice Splintering on Microphysics of Deep Convective Clouds Forming Under Different Aerosol Conditions: Simulations Using the Model With Spectral Bin Microphysics

Abstract: Observations during the Ice in Clouds Experiment‐Tropical (ICE‐T) field experiment show that the ice particles concentration in a developing deep convective clouds at the level of T = −15 °C reached about 500 L−1, that is, many orders higher than that of ice‐nucleating particle. To simulate microphysics of these clouds, the 2‐D Hebrew University Cloud model (HUCM) with spectral bin microphysics was used in which two main types of ice multiplication mechanisms were included in addition to the Hallet‐Mossop mech… Show more

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Cited by 15 publications
(7 citation statements)
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“…Individual experiments of freezing droplets reported the maximum fragmentation rate at temperatures between ~ -10 and -15 o C (Leisner et al, 2014;Lauber et al, 2018;Keinert et al, 2020). DS is found to be very efficient in vigorous convective updrafts (Lawson et al, 2015;Phillips et al, 2018;Qu et al, 2020), while remote sensing observations indicate that DS can be much more conducive to SIP in slightly supercooled Arctic MPCs than the wellknown HM process (Luke et al, 2021). This is in line with single-column simulations performed by Zhao et al (2021), but contradicts the findings of small-scale modeling studies suggesting that DS is ineffective in polar regions (Fu et al, 2019;Sotiropoulou et al, 2020).…”
Section: Introductionsupporting
confidence: 57%
See 1 more Smart Citation
“…Individual experiments of freezing droplets reported the maximum fragmentation rate at temperatures between ~ -10 and -15 o C (Leisner et al, 2014;Lauber et al, 2018;Keinert et al, 2020). DS is found to be very efficient in vigorous convective updrafts (Lawson et al, 2015;Phillips et al, 2018;Qu et al, 2020), while remote sensing observations indicate that DS can be much more conducive to SIP in slightly supercooled Arctic MPCs than the wellknown HM process (Luke et al, 2021). This is in line with single-column simulations performed by Zhao et al (2021), but contradicts the findings of small-scale modeling studies suggesting that DS is ineffective in polar regions (Fu et al, 2019;Sotiropoulou et al, 2020).…”
Section: Introductionsupporting
confidence: 57%
“…Parameterizations of this mechanism are implemented in small-scale models (Fridlind et al, 2007;Phillips et al, 2017a, b;Sotiropoulou et al, 2020Sotiropoulou et al, , 2021bSullivan et al, 2018a;Yano and Phillips, 2011;Yano et al, 2016), mesoscale models (Hoarau et al, 2018;Sullivan et al, 2018b;Qu et al, 2020;Sotiropoulou et al, 2021a;Dedekind et al, 2021) and global climate models (Zhao and Liu, 2021). These modeling studies followed several approaches to implement the effect of BR.…”
Section: Introductionmentioning
confidence: 99%
“…Although BR has been observed in polar conditions before (Rangno and Hobbs, 2001;Schwarzenboeck et al, 2009), this mechanism is currently not implemented in most weather prediction and climate models. The more advanced Phillips et al (2017a) parameterization produces realistic ICNCs in Antarctic clouds as long as a high rimed fraction is prescribed for the particles that undergo fracture, which is in agreement with Sotiropoulou et al (2020).…”
Section: Discussionmentioning
confidence: 99%
“…For example, the SNOWIE project is used to understand organic cloud dynamic and microphysical processes and addresses long-standing uncertainties regarding the effectiveness of organic cloud seeding [13,14]. Furthermore, the microphysical characteristics of clouds observed by aircraft play an important role in climate research and the determination of cloud parameterization schemes in numerical models [15][16][17]. In addition, remote sensing data, such as radar and satellites, are more helpful to evaluate the precipitation enhancement effectiveness through the value change of cloud parameters between pre-and post-cloud seeding.…”
Section: Related Workmentioning
confidence: 99%