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Vivek Sant Group Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6- HAM and previously developed aspects (entrainment, PBL clouds, shallow convection) Philipp Reutter/Betty Croft: aerosol processing and scavenging of aerosols Ana Sesartic: bioaersols and their possible importance as ice nuclei (IN) Vivek Sant: drizzle and giant CCN Miriam Kübbeler: heterogeneous vs. homogeneous freezing in cirrus clouds Sebastian Bretl: possible influence of aerosols on tropical cyclones

Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

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Page 1: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Vivek Sant Group Meeting

ECHAM activities – Ulrike Lohmann’s group

1February 1, 2011

• Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed aspects (entrainment, PBL clouds, shallow convection)

• Philipp Reutter/Betty Croft: aerosol processing and scavenging of aerosols

• Ana Sesartic: bioaersols and their possible importance as ice nuclei (IN)

• Vivek Sant: drizzle and giant CCN• Miriam Kübbeler: heterogeneous vs. homogeneous

freezing in cirrus clouds• Sebastian Bretl: possible influence of aerosols on

tropical cyclones

Page 2: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Reference scavenging ratios changed following a study in the Arctic study by Bourgeious and Bey (2011).

Impact of wet scavenging on global aerosol and cloudproperties in ECHAM5 (Philipp Reutter)

Page 3: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Less cloud droplet number burden and less soluble nucleation and Aitken mode particles when scavenging ratios are reduced

Mechanism: Initially more aerosol particles. Nucleation of new particles impeded, more condensation of SO4

and organics on pre-existing particles. Coagulation and less new particle formation lead to a reduction

of the number mixing ratio of smallest modes.

Page 4: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Impact on clouds & radiation • small global impact

• regional impact suspected

Possible future research• models with dynamic

vegetation• regional modelling

• observations & lab studies

IACETH

Inst

itute

for A

tmo

sph

eri

c a

nd

Clim

ate

Sci

en

ce

Bacteria and fungal spores in ECHAM (Ana Sesartic)

Page 5: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Vivek Sant Group Meeting

Introducing a drizzle class in ECHAM5 (Vivek Sant)

5

today

future

Courtesy of R. Posselt

February 1, 2011

Bretherton et al., 2001

Page 6: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Impact of aerosols on cirrus clouds (Miriam Kübbeler)

Kärcher et al., JGR, 2006

Page 7: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Impact of aerosols on cirrus clouds (Miriam Kübbeler)

Page 8: Vivek SantGroup Meeting ECHAM activities – Ulrike Lohmann’s group 1 February 1, 2011 Sylvaine Ferrachat: Maintainance of ECHAM6-HAM and previously developed

Influence of aerosols on hurricanes? (Sebastian Bretl)