Matches in SemOpenAlex for { <https://semopenalex.org/work/W4366598501> ?p ?o ?g. }
- W4366598501 endingPage "4761" @default.
- W4366598501 startingPage "4741" @default.
- W4366598501 abstract "Abstract. Ice-nucleating particles (INPs) can initiate ice formation in clouds at temperatures above −38 ∘C through heterogeneous ice nucleation. As a result, INPs affect cloud microphysical and radiative properties, cloud lifetime, and precipitation behavior and thereby ultimately the Earth's climate. Yet, little is known regarding the sources, abundance and properties of INPs, especially in remote regions such as the Arctic. In this study, 2-year-long INP measurements (from July 2018 to September 2020) at Villum Research Station in northern Greenland are presented. A low-volume filter sampler was deployed to collect filter samples for offline INP analysis. An annual cycle of INP concentration (NINP) was observed, and the fraction of heat-labile INPs was found to be higher in months with low to no snow cover and lower in months when the surface was well covered in snow (> 0.8 m). Samples were categorized into three different types based only on the slope of their INP spectra, namely into summer, winter and mix type. For each of the types a temperature-dependent INP parameterization was derived, clearly different depending on the time of the year. Winter and summer types occurred only during their respective seasons and were seen 60 % of the time. The mixed type occurred in the remaining 40 % of the time throughout the year. April, May and November were found to be transition months. A case study comparing April 2019 and April 2020 was performed. The month of April was selected because a significant difference in NINP was observed during these two periods, with clearly higher NINP in April 2020. In parallel to the observed differences in NINP, also a higher cloud-ice fraction was observed in satellite data for April 2020, compared to April 2019. NINP in the case study period revealed no clear dependency on either meteorological parameters or different surface types which were passed by the collected air masses. Overall, the results suggest that the coastal regions of Greenland were the main sources of INPs in April 2019 and 2020, most likely including both local terrestrial and marine sources." @default.
- W4366598501 created "2023-04-23" @default.
- W4366598501 creator A5003663952 @default.
- W4366598501 creator A5019012504 @default.
- W4366598501 creator A5019229404 @default.
- W4366598501 creator A5044561727 @default.
- W4366598501 creator A5044740856 @default.
- W4366598501 creator A5070245627 @default.
- W4366598501 creator A5088973180 @default.
- W4366598501 date "2023-04-20" @default.
- W4366598501 modified "2023-10-17" @default.
- W4366598501 title "Ice-nucleating particles in northern Greenland: annual cycles, biological contribution and parameterizations" @default.
- W4366598501 cites W1485504984 @default.
- W4366598501 cites W1570025454 @default.
- W4366598501 cites W1599956401 @default.
- W4366598501 cites W1724008355 @default.
- W4366598501 cites W1783045389 @default.
- W4366598501 cites W1890193808 @default.
- W4366598501 cites W1964688613 @default.
- W4366598501 cites W1970590897 @default.
- W4366598501 cites W1993436181 @default.
- W4366598501 cites W2009225674 @default.
- W4366598501 cites W2015392579 @default.
- W4366598501 cites W2015489805 @default.
- W4366598501 cites W2015772592 @default.
- W4366598501 cites W2017808887 @default.
- W4366598501 cites W2017859469 @default.
- W4366598501 cites W2029321418 @default.
- W4366598501 cites W2038683022 @default.
- W4366598501 cites W2064721584 @default.
- W4366598501 cites W2066330972 @default.
- W4366598501 cites W2069633418 @default.
- W4366598501 cites W2075712895 @default.
- W4366598501 cites W2079636125 @default.
- W4366598501 cites W2093674996 @default.
- W4366598501 cites W2100289143 @default.
- W4366598501 cites W2100365896 @default.
- W4366598501 cites W2105286019 @default.
- W4366598501 cites W2112360250 @default.
- W4366598501 cites W2115716542 @default.
- W4366598501 cites W2122078149 @default.
- W4366598501 cites W2132281993 @default.
- W4366598501 cites W2134591556 @default.
- W4366598501 cites W2138672757 @default.
- W4366598501 cites W2139215874 @default.
- W4366598501 cites W2140569468 @default.
- W4366598501 cites W2141442289 @default.
- W4366598501 cites W2161587320 @default.
- W4366598501 cites W2162445884 @default.
- W4366598501 cites W2173562403 @default.
- W4366598501 cites W2174346177 @default.
- W4366598501 cites W2175438141 @default.
- W4366598501 cites W2210130261 @default.
- W4366598501 cites W2258730496 @default.
- W4366598501 cites W2296138349 @default.
- W4366598501 cites W2532818588 @default.
- W4366598501 cites W2573803757 @default.
- W4366598501 cites W2593887101 @default.
- W4366598501 cites W2609400731 @default.
- W4366598501 cites W2616871981 @default.
- W4366598501 cites W2741321093 @default.
- W4366598501 cites W2753669009 @default.
- W4366598501 cites W2761214405 @default.
- W4366598501 cites W2790696117 @default.
- W4366598501 cites W2795040534 @default.
- W4366598501 cites W2799647124 @default.
- W4366598501 cites W2808410171 @default.
- W4366598501 cites W2891598053 @default.
- W4366598501 cites W2893278979 @default.
- W4366598501 cites W2899669666 @default.
- W4366598501 cites W2904220286 @default.
- W4366598501 cites W2908424681 @default.
- W4366598501 cites W2922761564 @default.
- W4366598501 cites W2929357723 @default.
- W4366598501 cites W2945049751 @default.
- W4366598501 cites W2946668812 @default.
- W4366598501 cites W2954934874 @default.
- W4366598501 cites W2959690709 @default.
- W4366598501 cites W2982400600 @default.
- W4366598501 cites W2996318325 @default.
- W4366598501 cites W3003596193 @default.
- W4366598501 cites W3004910872 @default.
- W4366598501 cites W3015542976 @default.
- W4366598501 cites W3034228277 @default.
- W4366598501 cites W3035332714 @default.
- W4366598501 cites W3037814288 @default.
- W4366598501 cites W3086814589 @default.
- W4366598501 cites W3107996900 @default.
- W4366598501 cites W3114923743 @default.
- W4366598501 cites W3135669282 @default.
- W4366598501 cites W3144011056 @default.
- W4366598501 cites W3180850803 @default.
- W4366598501 cites W4210364008 @default.
- W4366598501 cites W4210804024 @default.
- W4366598501 cites W4220749105 @default.
- W4366598501 cites W4234397917 @default.
- W4366598501 cites W4283160489 @default.
- W4366598501 cites W4292865744 @default.