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• W4200495503 endingPage "18053" @default.
• W4200495503 startingPage "18029" @default.
• W4200495503 abstract "Abstract. The ice phase in mixed-phase clouds has a pivotal role in global precipitation formation as well as for Earth's radiative budget. Above 235 K, sparse particles with the special ability to initiate ice formation, ice-nucleating particles (INPs), are responsible for primary ice formation within these clouds. Mineral dust has been found to be one of the most abundant INPs in the atmosphere at temperatures colder than 258 K. However, the extent of the abundance and distribution of INPs remains largely unknown. To better constrain and quantify the impact of mineral dust on ice nucleation, we investigate the frequency of Saharan dust events (SDEs) and their contribution to the INP number concentration at 243 K and at a saturation ratio with respect to liquid water (Sw) of 1.04 at the High Altitude Research Station Jungfraujoch (JFJ; 3580 m a.s.l.) from February to December 2020. Using the single-scattering albedo Ångström exponent retrieved from a nephelometer and an Aethalometer, satellite-retrieved dust mass concentrations, simulated tropospheric residence times, and the attenuated backscatter signal from a ceilometer as proxies, we detected 26 SDEs, which in total contributed to 17 % of the time span analyzed. We found every SDE to show an increase in median INP concentrations compared to those of all non-SDE periods; however, they were not always statistically significant. Median INP concentrations of individual SDEs spread between 1.7 and 161 INP std L−1 and thus 2 orders of magnitude. In the entire period analyzed, 74.7 ± 0.2 % of all INPs were measured during SDEs. Based on satellite-retrieved dust mass concentrations, we argue that mineral dust is also present at JFJ outside of SDEs but at much lower concentrations, thus still contributing to the INP population. We estimate that 97 % of all INPs active in the immersion mode at 243 K and Sw=1.04 at JFJ are dust particles. Overall, we found INP number concentrations to follow a leptokurtic lognormal frequency distribution. We found the INP number concentrations during SDEs to correlate with the ceilometer backscatter signals from a ceilometer located 4.5 km north of JFJ and 1510 m lower in altitude, thus scanning the air masses at the same altitude as JFJ. Using the European ceilometer network allows us to study the atmospheric pathway of mineral dust plumes over a large domain, which we demonstrate in two case studies. These studies showed that mineral dust plumes form ice crystals at cirrus altitudes, which then sediment to lower altitudes. Upon sublimation in dryer air layers, the residual particles are left potentially pre-activated. Future improvements to the sampling lines of INP counters are required to study whether these particles are indeed pre-activated, leading to larger INP number concentrations than reported here." @default.
• W4200495503 created "2021-12-31" @default.
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• W4200495503 date "2021-12-09" @default.
• W4200495503 modified "2023-10-03" @default.
• W4200495503 title "The contribution of Saharan dust to the ice-nucleating particle concentrations at the High Altitude Station Jungfraujoch (3580 m a.s.l.), Switzerland" @default.
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• W4200495503 cites W1587101236 @default.
• W4200495503 cites W1613795631 @default.
• W4200495503 cites W1669255424 @default.
• W4200495503 cites W1797279564 @default.
• W4200495503 cites W1890193808 @default.
• W4200495503 cites W1974930472 @default.
• W4200495503 cites W1976176506 @default.
• W4200495503 cites W1988186603 @default.
• W4200495503 cites W1989377335 @default.
• W4200495503 cites W1993133049 @default.
• W4200495503 cites W1993436181 @default.
• W4200495503 cites W1998647656 @default.
• W4200495503 cites W2017808887 @default.
• W4200495503 cites W2019723114 @default.
• W4200495503 cites W2029739915 @default.
• W4200495503 cites W2033391591 @default.
• W4200495503 cites W2036168723 @default.
• W4200495503 cites W2049076855 @default.
• W4200495503 cites W2050647958 @default.
• W4200495503 cites W2053898969 @default.
• W4200495503 cites W2066330972 @default.
• W4200495503 cites W2067094074 @default.
• W4200495503 cites W2075162893 @default.
• W4200495503 cites W2075712895 @default.
• W4200495503 cites W2085934640 @default.
• W4200495503 cites W2093674996 @default.
• W4200495503 cites W2105930044 @default.
• W4200495503 cites W2112360250 @default.
• W4200495503 cites W2115241739 @default.
• W4200495503 cites W2115869946 @default.
• W4200495503 cites W2118842843 @default.
• W4200495503 cites W2132077964 @default.
• W4200495503 cites W2135419069 @default.
• W4200495503 cites W2139742091 @default.
• W4200495503 cites W2142442494 @default.
• W4200495503 cites W2144991971 @default.
• W4200495503 cites W2146288844 @default.
• W4200495503 cites W2147067266 @default.
• W4200495503 cites W2149965517 @default.
• W4200495503 cites W2153571463 @default.
• W4200495503 cites W2153664297 @default.
• W4200495503 cites W2161642910 @default.
• W4200495503 cites W2162509780 @default.
• W4200495503 cites W2258185802 @default.
• W4200495503 cites W2285173847 @default.
• W4200495503 cites W2299477301 @default.
• W4200495503 cites W2301974363 @default.
• W4200495503 cites W2302598575 @default.
• W4200495503 cites W2323666233 @default.
• W4200495503 cites W2345352245 @default.
• W4200495503 cites W2416701218 @default.
• W4200495503 cites W2511008135 @default.
• W4200495503 cites W2560091048 @default.
• W4200495503 cites W2580528271 @default.
• W4200495503 cites W2753669009 @default.
• W4200495503 cites W2808410171 @default.
• W4200495503 cites W2865221093 @default.
• W4200495503 cites W2888113229 @default.
• W4200495503 cites W2891817162 @default.
• W4200495503 cites W2927736690 @default.
• W4200495503 cites W2945423688 @default.
• W4200495503 cites W2946329786 @default.
• W4200495503 cites W2958066056 @default.
• W4200495503 cites W2988794397 @default.
• W4200495503 cites W2994648189 @default.
• W4200495503 cites W3004910872 @default.
• W4200495503 cites W3041185276 @default.
• W4200495503 cites W3049469118 @default.
• W4200495503 cites W3086814589 @default.
• W4200495503 cites W3093462351 @default.
• W4200495503 cites W3097392967 @default.
• W4200495503 cites W3114923743 @default.
• W4200495503 cites W3133048246 @default.
• W4200495503 cites W3191370622 @default.
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• W4200495503 doi "https://doi.org/10.5194/acp-21-18029-2021" @default.
• W4200495503 hasPublicationYear "2021" @default.
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