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全球变暖与亚洲季风变化国际研讨会第一轮通知（International Workshop on the Asian Monsoon in a Warmer World）
全球变暖 亚洲季风变化 国际研讨会 第一轮通知
2017/3/16
Monsoon is an important component of the Earth’s climate system. It interacts with oceans, land, and the cryosphere and exerts far-reaching impacts on regional and global climate and environment. The ...
International Workshop on the Asian Monsoon in a Warmer World
International Workshop the Asian Monsoon in a Warmer World
2017/3/9
Monsoon is an important component of the Earth’s climate system. It interacts with oceans, land, and the cryosphere and exerts far-reaching impacts on regional and global climate and environment. The ...
3rd Workshop on Atmospheric Composition and the Asian Monsoon (Acam) and 2nd Acam Training School
3rd Workshop Atmospheric Composition and the Asian Monsoon 2nd Acam Training School
2017/3/9
Following successful workshops in 2013 (Kathmandu) and 2015 (Bangkok), ACAM is a fully recognized international activity jointly sponsored by SPARC and IGAC. The third biennial workshop...
Think of the Sahara and you will conjure images of a vast desert landscape, with nothing but sand as far as the eye can see. But for a period of about 10,000 years, the Sahara was characterized ...
Anthropogenic Aerosols and the Weakening of the South Asian Summer Monsoon
Anthropogenic Aerosols the Weakening South Asian Summer Monsoon
2014/5/20
Observations show that South Asia underwent a widespread summertime drying during the second half of the 20th century, but it is unclear whether this trend was due to natural variations or human activ...
Earlier onset of the Indian monsoon in the late twentieth century: The role of anthropogenic aerosols
Indian monsoon late twentieth century anthropogenic aerosols
2014/5/20
The impact of the late twentieth century increase of anthropogenic aerosols on the Indian monsoon onset was investigated with a state-of-the-art climate model with fully interactive aerosols and chemi...
Variations in Mass of the PM10, PM2.5 and PM1 during the Monsoon and the Winter at New Delhi
Particulate matters Visibility Washout pattern Time-series variations Mean mass scavenging coefficient
2016/3/28
PM10, PM2.5 and PM1 mass concentrations have been measured at Delhi (28°35'N; 77°12'E) during the August to
December 2007. The running mean of PM10, PM2.5 and PM1 data shows large variations. The PM1...
The general circulation model precipitation bias over the southwestern equatorial Indian Ocean and its implications for simulating the South Asian monsoon
General circulation models South Asian monsoon Sea surface temperature gradient Precipitation SEA-SURFACE TEMPERATURE BOUNDARY-LAYER WINDS SUMMER MONSOON TROPICAL OCEANS SST GRADIENTS GLOBAL PRECIPITATION VARIABILITY ATMOSPHERE RAINFALL PREDICTABILITY
2014/5/20
Most of current general circulation models (GCMs) show a remarkable positive precipitation bias over the southwestern equatorial Indian Ocean (SWEIO), which can be thought of as a westward expansion o...
Impact of the East Asian summer monsoon on long-term variations in the acidity of summer precipitation in Central China
the East Asian summer monsoon long-term variations the acidity of summer precipitation Central China
2011/2/25
The acidity of precipitation has been observed at stations of the Acid Rain Monitoring Network run by the China Meteorological Administration (CMA-ARMN) since 1992. Previous studies have shown that di...
Characterization of non-methane hydrocarbons in Asian summer monsoon outflow observed by the CARIBIC aircraft
non-methane hydrocarbons Asian summer monsoon the CARIBIC aircraft
2011/1/20
Between April and December 2008 the CARIBIC commercial aircraft conducted monthly measurement flights between Frankfurt, Germany and Chennai, India. These flights covered the period of the Asian summe...
Transport of dust particles from the Bodélé region to the monsoon layer – AMMA case study of the 9–14 June 2006 period
dust particles the Bodélé region the monsoon layer the 9–14 June 2006 period
2011/1/20
Aerosol properties were measured during an airborne campaign experiment that took place in June 2006 in West Africa within the framework of the African Monsoon Multidisciplinary Analyses (AMMA). The g...
Chemical composition and aerosol size distribution of the middle mountain range in the Nepal Himalayas during the 2009 pre-monsoon season
Chemical composition aerosol size the middle mountain range the Nepal Himalayas the 2009 pre-monsoon season
2010/12/28
Aerosol particle number size distribution and chemical composition were measured at two low altitude sites, one urban and one relatively pristine valley, in Central Nepal during the 2009 pre-monsoon s...
Air mass origins influencing TTL chemical composition over West Africa during 2006 summer monsoon
Air mass origins TTL chemical composition West Africa 2006 summer monsoon
2010/11/30
Trace gas and aerosol data collected in the tropical tropopause layer (TTL) between 12–18.5 km by the M55 Geophysica aircraft as part of the SCOUT-AMMA campaign over West Africa during the summer mons...
Reply to comment by K. M. Lau and K. M. Kim on '"Elevated heat pump' hypothesis for the aerosol-monsoon hydroclimate link: 'Grounded' in observations?"
K. M. Lau and K. M. Kim Elevated heat pump aerosol-monsoon hydroclimate link in observations
2014/5/20
Lau and Kim‟s [2011, hereafter LK11] defense of the Elevated Heat Pump (EHP) hypothesis is weak. Nigam and Bollasina [2010, hereafter NB10] have assessed the viability of the EHP hyp...
The influence of biomass burning and transport on tropospheric composition over the tropical Atlantic Ocean and Equatorial Africa during the West African monsoon in 2006
biomass burning and transport tropospheric composition the tropical Atlantic Ocean and Equatorial Africa the West African monsoon
2010/10/21
Biomass burning (BB) in southern Africa is the largest emission source of CO and O3 precursors within Africa during the West African Monsoon (WAM) between June and August. The long range transport and...