SwePub
Sök i LIBRIS databas

  Utökad sökning

L773:1600 0889 OR L773:0280 6509
 

Sökning: L773:1600 0889 OR L773:0280 6509 > (2005-2009) > The radiative effec...

The radiative effect of an aged, internally mixed Arctic aerosol originating from lower-latitude biomass burning

Engvall, Ann-Christine (författare)
Strom, Johan (författare)
Tunved, Peter (författare)
Stockholms universitet,Institutionen för tillämpad miljövetenskap (ITM)
visa fler...
Krejci, Radovan (författare)
Stockholms universitet,Institutionen för tillämpad miljövetenskap (ITM)
Schlager, Hans (författare)
Minikin, Andreas (författare)
visa färre...
 (creator_code:org_t)
2009-01-01
2009
Engelska.
Ingår i: Tellus. Series B, Chemical and physical meteorology. - : Stockholm University Press. - 0280-6509 .- 1600-0889. ; 61:4, s. 677-684
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Arctic-haze layers and their radiative effects have been investigated previously in numerous studies as they are known to have an impact on the regional climate. In this study, we report on an event of an elevated aerosol layer, notably consisting of high-absorbing soot particles, observed in the European Arctic free troposphere the 2007 April 14 during the ASTAR 2007 campaign. The ca. 0.5 km vertically thick aerosol layer located at an altitude of around 3 km had a particle-size distribution mode around 250 nm diameter. In this study, we quantify the radiative effect aerosol layers have on the Arctic atmosphere by using in situ observations. Measurements of particles size segregated temperature stability using thermal denuders, indicate that the aerosol in the optically active size range was chemically internally mixed. In the plume, maximum observed absorption and scattering coefficients were 3 x 10(-6) and 20 x 10(-6) m(-1), respectively. Observed microphysical and optical properties were used to constrain calculations of heating rates of an internally mixed aerosol assuming two different surface albedos that represent snow/ice covered and open ocean. The average profile resulted in a heating rate in the layer of 0.2 K d(-1) for the high-albedo case and 0.15 K d(-1) for the low albedo case. This calculated dependence on albedo based on actual observations corroborates previous numerical simulations. The heating within the plume resulted in a measurable signal shown as an enhancement in the temperature of a few tenths of a degree. Although the origin of the aerosol plume could not unambiguously be determined, the microphysical properties of the aerosol had strong similarities with previously reported biomass burning plumes. With a changing climate, short-lived pollutants such as biomass plumes may become more frequent in the Arctic and have important radiative effects at regional scale.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Nyckelord

black carbon
particle-size
dependence
impact
soot
Svalbard
boreal
clouds
Brazil
state
Earth sciences
Geovetenskap

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Sök utanför SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy