Matches in SemOpenAlex for { <https://semopenalex.org/work/W1832011511> ?p ?o ?g. }
- W1832011511 endingPage "351" @default.
- W1832011511 startingPage "331" @default.
- W1832011511 abstract "Abstract A Lagrangian technique is developed to sample satellite data to quantify and understand factors controlling temporal changes in low-cloud properties (cloud cover, areal-mean liquid water path, and droplet concentration). Over 62 000 low-cloud scenes over the eastern subtropical/tropical oceans are sampled using the A-Train satellites. Horizontal wind fields at 925 hPa from the ERA-Interim are used to compute 24-h, two-dimensional, forward, boundary layer trajectories with trajectory locations starting on the CloudSat/CALIPSO track. Cloud properties from MODIS and AMSR-E are sampled at the trajectory start and end points, allowing for direct measurement of the temporal cloud evolution. The importance of various controls (here, boundary layer depth, lower-tropospheric stability, and precipitation) on cloud evolution is evaluated by comparing cloud evolution for different initial values of these controls. Viewing angle biases are removed and cloud anomalies (diurnal and seasonal cycles removed) are used throughout to quantify cloud evolution relative to the climatological-mean evolution. Cloud property anomalies show temporal changes similar to those expected for a stochastic red noise process, with linear relationships between initial anomalies and their mean 24-h changes. This creates a potential bias when comparing the evolutions of sets of trajectories with different initial anomalies; three methods are introduced and evaluated to account for this. Results provide statistically robust observational support for theoretical/modeling studies by showing that low clouds in deep boundary layers and under weak inversions are prone to break up. Precipitation shows a more complex and less statistically significant relationship with cloud breakup. Cloud cover in shallow precipitating boundary layers is more persistent than in deep precipitating boundary layers. Liquid water path and cloud droplet concentration decrease more rapidly for precipitating clouds and in deep boundary layers." @default.
- W1832011511 created "2016-06-24" @default.
- W1832011511 creator A5021955604 @default.
- W1832011511 creator A5073221405 @default.
- W1832011511 date "2015-12-30" @default.
- W1832011511 modified "2023-10-14" @default.
- W1832011511 title "Factors Controlling Low-Cloud Evolution over the Eastern Subtropical Oceans: A Lagrangian Perspective Using the A-Train Satellites" @default.
- W1832011511 cites W1965845688 @default.
- W1832011511 cites W1981413870 @default.
- W1832011511 cites W1990727484 @default.
- W1832011511 cites W1992746134 @default.
- W1832011511 cites W1994470279 @default.
- W1832011511 cites W1996256697 @default.
- W1832011511 cites W1999598849 @default.
- W1832011511 cites W2018942029 @default.
- W1832011511 cites W2029784610 @default.
- W1832011511 cites W2046281685 @default.
- W1832011511 cites W2047097077 @default.
- W1832011511 cites W2064943738 @default.
- W1832011511 cites W2072919312 @default.
- W1832011511 cites W2075931697 @default.
- W1832011511 cites W2091803649 @default.
- W1832011511 cites W2097625988 @default.
- W1832011511 cites W2098821440 @default.
- W1832011511 cites W2099645289 @default.
- W1832011511 cites W2116509823 @default.
- W1832011511 cites W2117245913 @default.
- W1832011511 cites W2121745948 @default.
- W1832011511 cites W2123130978 @default.
- W1832011511 cites W2127502931 @default.
- W1832011511 cites W2130900843 @default.
- W1832011511 cites W2137666472 @default.
- W1832011511 cites W2141526687 @default.
- W1832011511 cites W2147763048 @default.
- W1832011511 cites W2149890601 @default.
- W1832011511 cites W2150403226 @default.
- W1832011511 cites W2154894457 @default.
- W1832011511 cites W2158560528 @default.
- W1832011511 cites W2159897356 @default.
- W1832011511 cites W4211083409 @default.
- W1832011511 cites W4242020285 @default.
- W1832011511 cites W4249268861 @default.
- W1832011511 doi "https://doi.org/10.1175/jas-d-15-0193.1" @default.
- W1832011511 hasPublicationYear "2015" @default.
- W1832011511 type Work @default.
- W1832011511 sameAs 1832011511 @default.
- W1832011511 citedByCount "23" @default.
- W1832011511 countsByYear W18320115112016 @default.
- W1832011511 countsByYear W18320115112017 @default.
- W1832011511 countsByYear W18320115112018 @default.
- W1832011511 countsByYear W18320115112019 @default.
- W1832011511 countsByYear W18320115112020 @default.
- W1832011511 countsByYear W18320115112021 @default.
- W1832011511 countsByYear W18320115112022 @default.
- W1832011511 crossrefType "journal-article" @default.
- W1832011511 hasAuthorship W1832011511A5021955604 @default.
- W1832011511 hasAuthorship W1832011511A5073221405 @default.
- W1832011511 hasBestOaLocation W18320115111 @default.
- W1832011511 hasConcept C105795698 @default.
- W1832011511 hasConcept C107054158 @default.
- W1832011511 hasConcept C111919701 @default.
- W1832011511 hasConcept C121332964 @default.
- W1832011511 hasConcept C127313418 @default.
- W1832011511 hasConcept C1276947 @default.
- W1832011511 hasConcept C13662910 @default.
- W1832011511 hasConcept C153294291 @default.
- W1832011511 hasConcept C19269812 @default.
- W1832011511 hasConcept C197640229 @default.
- W1832011511 hasConcept C199194280 @default.
- W1832011511 hasConcept C206887242 @default.
- W1832011511 hasConcept C23302255 @default.
- W1832011511 hasConcept C2778516841 @default.
- W1832011511 hasConcept C33923547 @default.
- W1832011511 hasConcept C39432304 @default.
- W1832011511 hasConcept C41008148 @default.
- W1832011511 hasConcept C49204034 @default.
- W1832011511 hasConcept C51399673 @default.
- W1832011511 hasConcept C62649853 @default.
- W1832011511 hasConcept C79974875 @default.
- W1832011511 hasConcept C91586092 @default.
- W1832011511 hasConceptScore W1832011511C105795698 @default.
- W1832011511 hasConceptScore W1832011511C107054158 @default.
- W1832011511 hasConceptScore W1832011511C111919701 @default.
- W1832011511 hasConceptScore W1832011511C121332964 @default.
- W1832011511 hasConceptScore W1832011511C127313418 @default.
- W1832011511 hasConceptScore W1832011511C1276947 @default.
- W1832011511 hasConceptScore W1832011511C13662910 @default.
- W1832011511 hasConceptScore W1832011511C153294291 @default.
- W1832011511 hasConceptScore W1832011511C19269812 @default.
- W1832011511 hasConceptScore W1832011511C197640229 @default.
- W1832011511 hasConceptScore W1832011511C199194280 @default.
- W1832011511 hasConceptScore W1832011511C206887242 @default.
- W1832011511 hasConceptScore W1832011511C23302255 @default.
- W1832011511 hasConceptScore W1832011511C2778516841 @default.
- W1832011511 hasConceptScore W1832011511C33923547 @default.
- W1832011511 hasConceptScore W1832011511C39432304 @default.
- W1832011511 hasConceptScore W1832011511C41008148 @default.
- W1832011511 hasConceptScore W1832011511C49204034 @default.