Matches in SemOpenAlex for { <https://semopenalex.org/work/W1866219712> ?p ?o ?g. }
- W1866219712 endingPage "11,663" @default.
- W1866219712 startingPage "11,647" @default.
- W1866219712 abstract "[1] A recently developed new particle formation (NPF)-explicit version of the Weather Research and Forecasting Chemistry (WRF-chem) model can explicitly calculate the growth and sink of nucleated clusters with 20 aerosol size bins from 1 nm to 10 µm in diameter. In this study, the model was used to investigate spatial and temporal variations in NPF event frequency and the concentrations of aerosols (condensation nuclei, CN) and cloud condensation nuclei (CCN) within the boundary layer in East Asia in spring 2009. We found a distinct north-south contrast in the NPF frequency and mechanism in East Asia. NPF occurred mainly during limited periods over certain regions between 30° and 45°N (northeast China, Korea, and Japan, including regions around the active volcanoes Miyakejima and Sakurajima). In these latitudes, NPF was suppressed by high concentrations of preexisting particles under stagnant air conditions associated with high-pressure systems, although nucleation occurred more extensively during most of the simulation period. In contrast, south of 30°N, nucleation and NPF were both infrequent because of low SO2 emissions and H2SO4 concentrations. The period-averaged NPF frequency at 30°–45°N was three times that at 20°–30°N. This north-south contrast in NPF frequency was validated by surface measurements in outflow regions of East Asia. The simulated period- and domain-averaged contribution of secondary particles was estimated to be 44% for CN (>10 nm) and 26% for CCN at a supersaturation of 1.0%, though the contribution was highly sensitive to the amount and size distribution of primary aerosol emissions and the rate coefficient of the nucleation parameterization." @default.
- W1866219712 created "2016-06-24" @default.
- W1866219712 creator A5003987428 @default.
- W1866219712 creator A5018167585 @default.
- W1866219712 creator A5038082780 @default.
- W1866219712 creator A5041891963 @default.
- W1866219712 creator A5046506553 @default.
- W1866219712 creator A5046558730 @default.
- W1866219712 creator A5054548770 @default.
- W1866219712 creator A5056263999 @default.
- W1866219712 creator A5061145829 @default.
- W1866219712 creator A5070892078 @default.
- W1866219712 date "2013-10-17" @default.
- W1866219712 modified "2023-10-16" @default.
- W1866219712 title "Spatial and temporal variations of new particle formation in East Asia using an NPF-explicit WRF-chem model: North-south contrast in new particle formation frequency" @default.
- W1866219712 cites W1488605052 @default.
- W1866219712 cites W1541967971 @default.
- W1866219712 cites W1544276658 @default.
- W1866219712 cites W1931020421 @default.
- W1866219712 cites W1968177626 @default.
- W1866219712 cites W1968880292 @default.
- W1866219712 cites W1969008278 @default.
- W1866219712 cites W1972151806 @default.
- W1866219712 cites W1974521901 @default.
- W1866219712 cites W1975479292 @default.
- W1866219712 cites W1983279359 @default.
- W1866219712 cites W1984437578 @default.
- W1866219712 cites W1987864526 @default.
- W1866219712 cites W1994059485 @default.
- W1866219712 cites W1994825092 @default.
- W1866219712 cites W1994848639 @default.
- W1866219712 cites W2001952362 @default.
- W1866219712 cites W2004217539 @default.
- W1866219712 cites W2007841777 @default.
- W1866219712 cites W2008092456 @default.
- W1866219712 cites W2008196945 @default.
- W1866219712 cites W2011254556 @default.
- W1866219712 cites W2012086419 @default.
- W1866219712 cites W2012165084 @default.
- W1866219712 cites W2012381279 @default.
- W1866219712 cites W2012780281 @default.
- W1866219712 cites W2013350969 @default.
- W1866219712 cites W2013700001 @default.
- W1866219712 cites W2015349974 @default.
- W1866219712 cites W2016333953 @default.
- W1866219712 cites W2020371347 @default.
- W1866219712 cites W2022762325 @default.
- W1866219712 cites W2024001260 @default.
- W1866219712 cites W2026275622 @default.
- W1866219712 cites W2027405760 @default.
- W1866219712 cites W2027483555 @default.
- W1866219712 cites W2027734276 @default.
- W1866219712 cites W2028782877 @default.
- W1866219712 cites W2030875415 @default.
- W1866219712 cites W2030908262 @default.
- W1866219712 cites W2031110874 @default.
- W1866219712 cites W2035659804 @default.
- W1866219712 cites W2036180834 @default.
- W1866219712 cites W2036262211 @default.
- W1866219712 cites W2040006625 @default.
- W1866219712 cites W2042860652 @default.
- W1866219712 cites W2045030500 @default.
- W1866219712 cites W2045587156 @default.
- W1866219712 cites W2046550951 @default.
- W1866219712 cites W2047391056 @default.
- W1866219712 cites W2051390802 @default.
- W1866219712 cites W2053760139 @default.
- W1866219712 cites W2053997985 @default.
- W1866219712 cites W2054502311 @default.
- W1866219712 cites W2055195045 @default.
- W1866219712 cites W2055381129 @default.
- W1866219712 cites W2055704395 @default.
- W1866219712 cites W2056981114 @default.
- W1866219712 cites W2061318805 @default.
- W1866219712 cites W2066673620 @default.
- W1866219712 cites W2067209936 @default.
- W1866219712 cites W2067318157 @default.
- W1866219712 cites W2072692927 @default.
- W1866219712 cites W2077561616 @default.
- W1866219712 cites W2078592413 @default.
- W1866219712 cites W2079190988 @default.
- W1866219712 cites W2079600028 @default.
- W1866219712 cites W2081649906 @default.
- W1866219712 cites W2082745110 @default.
- W1866219712 cites W2087140992 @default.
- W1866219712 cites W2087367872 @default.
- W1866219712 cites W2092866358 @default.
- W1866219712 cites W2095461364 @default.
- W1866219712 cites W2097905719 @default.
- W1866219712 cites W2099168714 @default.
- W1866219712 cites W2099272050 @default.
- W1866219712 cites W2102948292 @default.
- W1866219712 cites W2105565190 @default.
- W1866219712 cites W2106179545 @default.
- W1866219712 cites W2110123713 @default.
- W1866219712 cites W2111259677 @default.
- W1866219712 cites W2113813921 @default.
- W1866219712 cites W2114829375 @default.