FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2790210930> ?p ?o ?g. }

• W2790210930 endingPage "2612" @default.
• W2790210930 startingPage "2597" @default.
• W2790210930 abstract "A-train satellite data, acquired during the Calbuco volcano (Chile) sub-Plinian eruption in April 2015, are discussed to explore the complementarity of spaceborne observations in the microwave (MW), thermal infrared (TIR), and visible wavelengths for both near-source plume and distal ash clouds. The analysis shows that TIR-based detection techniques are not suitable near the volcanic vent where rising convective columns are associated with large optical depths. Detection and parametric estimates of near-source tephra mass loading and plume height from MW radiometric data, available 69 min after the eruption onset, are proposed. Results indicate a maximum plume altitude of about 21 km above the sea level and an ash mass of $3.65 times 10^{10}$ kg, in agreement with mass values obtained from empirical formulas, but less than proximal–distal mass deposit of $1.86 times 10^{11}$ kg. This discrepancy may be explained by extrapolating Advanced Technology Microwave Sounder-based estimates to 6 h, thus obtaining a total mass of about $1.90 times 10^{11}$ kg. Distal volcanic cloud retrievals are derived from TIR imagery and results show a good agreement between Moderate-Resolution Imaging Spectroradiometer (MODIS) and Visible Infrared Imaging Radiometer Suite (VIIRS) retrievals of total mass taking into account the overpass time shift. If only the overlapping pixels between MODIS and VIIRS are considered, the respective estimates are $1.90 times 10^{9}$ kg and $1.80 times 10^{9}$ kg. TIR radiometric estimates of distal ash cloud height and mass loadings are also compared with Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations lidar retrievals. For low-to-medium optically thick ash cloud, average Cloud-Aerosol Lidar with Orthogonal Polarization-derived mass loading is about 0.8 g/m2 against 0.4 g/m2 from VIIRS and 1.4 g/m2 from MODIS." @default.
• W2790210930 created "2018-03-29" @default.
• W2790210930 creator A5038068921 @default.
• W2790210930 creator A5039674271 @default.
• W2790210930 creator A5043070577 @default.
• W2790210930 creator A5044836011 @default.
• W2790210930 creator A5059660583 @default.
• W2790210930 creator A5063760127 @default.
• W2790210930 creator A5071120785 @default.
• W2790210930 creator A5083707123 @default.
• W2790210930 date "2018-05-01" @default.
• W2790210930 modified "2023-09-30" @default.
• W2790210930 title "Multisatellite Multisensor Observations of a Sub-Plinian Volcanic Eruption: The 2015 Calbuco Explosive Event in Chile" @default.
• W2790210930 cites W1500428130 @default.
• W2790210930 cites W1606148469 @default.
• W2790210930 cites W1830081507 @default.
• W2790210930 cites W1845410120 @default.
• W2790210930 cites W1993523569 @default.
• W2790210930 cites W2001892132 @default.
• W2790210930 cites W2038963893 @default.
• W2790210930 cites W2040073534 @default.
• W2790210930 cites W2040321354 @default.
• W2790210930 cites W2040543587 @default.
• W2790210930 cites W2051481444 @default.
• W2790210930 cites W2053870625 @default.
• W2790210930 cites W2056377465 @default.
• W2790210930 cites W2075887614 @default.
• W2790210930 cites W2077218413 @default.
• W2790210930 cites W2089813147 @default.
• W2790210930 cites W2091233539 @default.
• W2790210930 cites W2096033560 @default.
• W2790210930 cites W2096548910 @default.
• W2790210930 cites W2104900072 @default.
• W2790210930 cites W2115307016 @default.
• W2790210930 cites W2125855972 @default.
• W2790210930 cites W2130805251 @default.
• W2790210930 cites W2137837432 @default.
• W2790210930 cites W2143580731 @default.
• W2790210930 cites W2144991971 @default.
• W2790210930 cites W2149965206 @default.
• W2790210930 cites W2154612353 @default.
• W2790210930 cites W2156645902 @default.
• W2790210930 cites W2161669521 @default.
• W2790210930 cites W2163313249 @default.
• W2790210930 cites W2164924179 @default.
• W2790210930 cites W2237749520 @default.
• W2790210930 cites W2278573025 @default.
• W2790210930 cites W2295340834 @default.
• W2790210930 cites W2338164468 @default.
• W2790210930 cites W2346724103 @default.
• W2790210930 cites W2479033801 @default.
• W2790210930 cites W2575311508 @default.
• W2790210930 cites W4240733927 @default.
• W2790210930 doi "https://doi.org/10.1109/tgrs.2017.2769003" @default.
• W2790210930 hasPublicationYear "2018" @default.
• W2790210930 type Work @default.
• W2790210930 sameAs 2790210930 @default.
• W2790210930 citedByCount "13" @default.
• W2790210930 countsByYear W27902109302019 @default.
• W2790210930 countsByYear W27902109302020 @default.
• W2790210930 countsByYear W27902109302021 @default.
• W2790210930 countsByYear W27902109302022 @default.
• W2790210930 countsByYear W27902109302023 @default.
• W2790210930 crossrefType "journal-article" @default.
• W2790210930 hasAuthorship W2790210930A5038068921 @default.
• W2790210930 hasAuthorship W2790210930A5039674271 @default.
• W2790210930 hasAuthorship W2790210930A5043070577 @default.
• W2790210930 hasAuthorship W2790210930A5044836011 @default.
• W2790210930 hasAuthorship W2790210930A5059660583 @default.
• W2790210930 hasAuthorship W2790210930A5063760127 @default.
• W2790210930 hasAuthorship W2790210930A5071120785 @default.
• W2790210930 hasAuthorship W2790210930A5083707123 @default.
• W2790210930 hasConcept C109902934 @default.
• W2790210930 hasConcept C120806208 @default.
• W2790210930 hasConcept C121332964 @default.
• W2790210930 hasConcept C127313418 @default.
• W2790210930 hasConcept C146348940 @default.
• W2790210930 hasConcept C154238967 @default.
• W2790210930 hasConcept C165205528 @default.
• W2790210930 hasConcept C166957645 @default.
• W2790210930 hasConcept C176943803 @default.
• W2790210930 hasConcept C205649164 @default.
• W2790210930 hasConcept C2779662365 @default.
• W2790210930 hasConcept C62520636 @default.
• W2790210930 hasConcept C62649853 @default.
• W2790210930 hasConcept C95869378 @default.
• W2790210930 hasConceptScore W2790210930C109902934 @default.
• W2790210930 hasConceptScore W2790210930C120806208 @default.
• W2790210930 hasConceptScore W2790210930C121332964 @default.
• W2790210930 hasConceptScore W2790210930C127313418 @default.
• W2790210930 hasConceptScore W2790210930C146348940 @default.
• W2790210930 hasConceptScore W2790210930C154238967 @default.
• W2790210930 hasConceptScore W2790210930C165205528 @default.
• W2790210930 hasConceptScore W2790210930C166957645 @default.
• W2790210930 hasConceptScore W2790210930C176943803 @default.
• W2790210930 hasConceptScore W2790210930C205649164 @default.
• W2790210930 hasConceptScore W2790210930C2779662365 @default.
• W2790210930 hasConceptScore W2790210930C62520636 @default.

• next