FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3092971366> ?p ?o ?g. }

• W3092971366 endingPage "3971" @default.
• W3092971366 startingPage "3949" @default.
• W3092971366 abstract "Abstract. Supercooled clouds substantially impact polar surface energy budgets, but large-scale models often underestimate their occurrence, which motivates accurately establishing metrics of basic processes. An analysis of long-term measurements at Utqiaġvik, Alaska, and McMurdo Station, Antarctica, combines lidar-validated use of soundings to identify supercooled cloud layers and colocated ground-based profiling radar measurements to quantify cloud base precipitation. We find that more than 85 % (75 %) of sampled supercooled layers are precipitating over the Arctic (Antarctic) site, with more than 75 % (50 %) precipitating continuously to the surface. Such high frequencies can be reconciled with substantially lesser spaceborne estimates by considering differences in radar hydrometeor detection sensitivity. While ice precipitation into supercooled clouds from aloft is common, we also find that the great majority of supercooled cloud layers without ice falling into them are themselves continuously generating precipitation. Such sustained primary ice formation is consistent with continuous activation of immersion-mode ice-nucleating particles (INPs), suggesting that supercooled cloud formation is a principal gateway to ice formation at temperatures greater than ∼-38 ∘C over polar regions. The prevalence of weak precipitation fluxes is also consistent with supercooled cloud longevity and with well-observed and widely simulated case studies. An analysis of colocated microwave radiometer retrievals suggests that weak precipitation fluxes can be nonetheless consequential to moisture budgets for supercooled clouds owing to small liquid water paths. The results here also demonstrate that the observed abundance of mixed-phase clouds can vary substantially with instrument sensitivity and methodology. Finally, we suggest that these ground-based precipitation rate statistics offer valuable guidance for improving the representation of polar cloud processes in large-scale models." @default.
• W3092971366 created "2020-10-22" @default.
• W3092971366 creator A5012458276 @default.
• W3092971366 creator A5028514038 @default.
• W3092971366 creator A5033429868 @default.
• W3092971366 creator A5049444999 @default.
• W3092971366 creator A5060008195 @default.
• W3092971366 creator A5089514641 @default.
• W3092971366 date "2021-03-17" @default.
• W3092971366 modified "2023-10-16" @default.
• W3092971366 title "The prevalence of precipitation from polar supercooled clouds" @default.
• W3092971366 cites W119095405 @default.
• W3092971366 cites W1540910639 @default.
• W3092971366 cites W1570025454 @default.
• W3092971366 cites W1613795631 @default.
• W3092971366 cites W1725227087 @default.
• W3092971366 cites W1868358499 @default.
• W3092971366 cites W1890193808 @default.
• W3092971366 cites W1918051004 @default.
• W3092971366 cites W1922593318 @default.
• W3092971366 cites W1965606220 @default.
• W3092971366 cites W1971635295 @default.
• W3092971366 cites W1973363367 @default.
• W3092971366 cites W1975534319 @default.
• W3092971366 cites W1978773894 @default.
• W3092971366 cites W1984031366 @default.
• W3092971366 cites W1989988408 @default.
• W3092971366 cites W1992981130 @default.
• W3092971366 cites W2002898709 @default.
• W3092971366 cites W2005766237 @default.
• W3092971366 cites W2010554983 @default.
• W3092971366 cites W2020306791 @default.
• W3092971366 cites W2022839575 @default.
• W3092971366 cites W2029322549 @default.
• W3092971366 cites W2029376422 @default.
• W3092971366 cites W2040574312 @default.
• W3092971366 cites W2048051513 @default.
• W3092971366 cites W2051487741 @default.
• W3092971366 cites W2056575570 @default.
• W3092971366 cites W2058897832 @default.
• W3092971366 cites W2073298425 @default.
• W3092971366 cites W2077712623 @default.
• W3092971366 cites W2086190558 @default.
• W3092971366 cites W2090735862 @default.
• W3092971366 cites W2095702361 @default.
• W3092971366 cites W2097535990 @default.
• W3092971366 cites W2100365896 @default.
• W3092971366 cites W2101977619 @default.
• W3092971366 cites W2116239281 @default.
• W3092971366 cites W2118326608 @default.
• W3092971366 cites W2118908291 @default.
• W3092971366 cites W2119525553 @default.
• W3092971366 cites W2122518875 @default.
• W3092971366 cites W2124202701 @default.
• W3092971366 cites W2133868929 @default.
• W3092971366 cites W2134426855 @default.
• W3092971366 cites W2135239023 @default.
• W3092971366 cites W2139215874 @default.
• W3092971366 cites W2140771520 @default.
• W3092971366 cites W2143117507 @default.
• W3092971366 cites W2145281096 @default.
• W3092971366 cites W2149355498 @default.
• W3092971366 cites W2150800280 @default.
• W3092971366 cites W2152916584 @default.
• W3092971366 cites W2162703778 @default.
• W3092971366 cites W2164394722 @default.
• W3092971366 cites W2168543820 @default.
• W3092971366 cites W2175511559 @default.
• W3092971366 cites W2319504665 @default.
• W3092971366 cites W2336754626 @default.
• W3092971366 cites W23839035 @default.
• W3092971366 cites W2462452433 @default.
• W3092971366 cites W2511008135 @default.
• W3092971366 cites W2593671740 @default.
• W3092971366 cites W2593887101 @default.
• W3092971366 cites W2625397172 @default.
• W3092971366 cites W2759967286 @default.
• W3092971366 cites W2767342244 @default.
• W3092971366 cites W2769525580 @default.
• W3092971366 cites W2784555771 @default.
• W3092971366 cites W2788281977 @default.
• W3092971366 cites W2788723540 @default.
• W3092971366 cites W2788885872 @default.
• W3092971366 cites W2794971334 @default.
• W3092971366 cites W2800683319 @default.
• W3092971366 cites W2804035800 @default.
• W3092971366 cites W2808792444 @default.
• W3092971366 cites W2896713802 @default.
• W3092971366 cites W2898524214 @default.
• W3092971366 cites W2899361914 @default.
• W3092971366 cites W2904220286 @default.
• W3092971366 cites W2908111793 @default.
• W3092971366 cites W2911944927 @default.
• W3092971366 cites W2916685104 @default.
• W3092971366 cites W2936674116 @default.
• W3092971366 cites W2937264792 @default.
• W3092971366 cites W2945319266 @default.
• W3092971366 cites W2950570551 @default.

• next