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Explore the annual variation of aerosol size distribution, light absorption coefficient, and more at Mount Waliguan in inland China. Discover the impact of local topography and air mass patterns on aerosol characteristics.
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DMPS measurements at Mount Waliguan, inland China Niku Kivekäs NOSA 9.11.2007
Thanks and acknowledgements • Finnish Meteorological Institute: • Heikki Lihavainen • Mika Komppula • Veli-Matti Kerminen • Yrjö Viisanen • Chinese Academy of Meteorological Sciences: • Jun-Ying Sun • Ming-Jin Zhan • Funding & Other: • Academy of Finland • Mount Waliguan Research Station Ilmatieteen laitos / PowerPoint ohjeistus
Mt Waliguan GAW station 36.283°N 100.900°E 3810 m a.s.l. (Highest Global GAW) Ilmatieteen laitos / PowerPoint ohjeistus
Mt Waliguan surroundings Ilmatieteen laitos / PowerPoint ohjeistus
Climate at Mount Waliguan Annual variation of T Seasonal wind distribution Ilmatieteen laitos / PowerPoint ohjeistus
Measurements at Mt Waliguan • Aerosol measurements: • Size distribution (2005-2007) • DMPS (9-600 nm) • CPC • Light absorption coefficient • Optical depth • Other measurements: • Greenhouse gases • Meteorology • Precipitation chemistry • Solar radiation • Ozone • Reactive gases Ilmatieteen laitos / PowerPoint ohjeistus
Mt waliguan data coverage Ilmatieteen laitos / PowerPoint ohjeistus
Annual variation of Np(mode) Ilmatieteen laitos / PowerPoint ohjeistus
Daily variation 1, Winter Ilmatieteen laitos / PowerPoint ohjeistus
Daily variation 2, Spring Ilmatieteen laitos / PowerPoint ohjeistus
Daily variation 3, Summer Ilmatieteen laitos / PowerPoint ohjeistus
Daily variation 4, Fall Ilmatieteen laitos / PowerPoint ohjeistus
Clustering the size distributions Ilmatieteen laitos / PowerPoint ohjeistus
Size distribution clusters Ilmatieteen laitos / PowerPoint ohjeistus
Sectors for trajectory analysis Sector 1 North Sector 4 Deserts Sector 2 China Sector 3 India / Tibet Ilmatieteen laitos / PowerPoint ohjeistus
Size distribution clusters from each sector (-24h) Ilmatieteen laitos / PowerPoint ohjeistus
Wind roses for each cluster Ilmatieteen laitos / PowerPoint ohjeistus
Conclusions • Air at Mt Waliguan has approximately 2300 particles (9-600 nm) / cm3 (at ambient pressure). • There is no clear seasonal pattern in Np. • There is a daily pattern of Np in nucleation (and partly Aitken) mode. The pattern is present at all seasons. • There is an air mass pattern in Np and the shape of the size distributions. Western air masses contain smaller particles than eastern air masses. • Local topography affects wind direction making the wind rose analysis different from trajectory analysis Ilmatieteen laitos / PowerPoint ohjeistus
Thank you for your attention Ilmatieteen laitos / PowerPoint ohjeistus
Size distribution types seasonally Ilmatieteen laitos / PowerPoint ohjeistus
Size distribution types monthly Ilmatieteen laitos / PowerPoint ohjeistus
Air mass history vs wind direction Ilmatieteen laitos / PowerPoint ohjeistus
Reasons for missing data 2-3 / 2006 7-8 / 2006 Ilmatieteen laitos / PowerPoint ohjeistus