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en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker [2024/07/06 19:28] – draft created Jürgen Vollmeren:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker [2024/09/02 10:37] (current) – add core questions Jürgen Vollmer
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-~~NOTOC~~+~~NOTOC~~  
 ====== Aerosols as climate drivers ====== ====== Aerosols as climate drivers ======
 +
 +
 +<WRAP group>
 +<WRAP half column>
  
 ===== Mira Pöhlker  ===== ===== Mira Pöhlker  =====
  
-> [[https://www.vetmed.uni-leipzig.de/personenprofil/mitarbeiter/prof-dr-martin-pfeffer|Institut für Tierhygiene und Öffentliches Veterinärwesen]], Universität Leipzig+> [[https://www.tropos.de/institut/ueber-uns/mitarbeitende/mira-poehlker|Head]] of the Department for [[https://www.tropos.de/institut/abteilungen/experimentelle-aerosol-und-wolkenmikrophysik|Atmospheric Microphysics]] 
 +> [[https://www.tropos.de/en/|Leibniz Institute for Tropospheric Research]]
  
  
-==== Abstract ====+==== Core Questions ====
  
 +  * What is the role of aerosols and clouds in the climate system?
 +  * How do their properties change due to human and natural impact?
  
-<WRAP group> 
-<WRAP half column> 
-<wrap lo center> 
-{{  .:2025-01-16_poehlker:aerosol-particles-bw.png?nolink  |}} 
  
-Exemplary illustrations of atmospheric particles and bioaerosols. Fig. 1 of [1]. +==== Abstract ====
-</wrap>+
  
-In addition to long-lived climate drivers such as CO2, aerosol particles (cf. figure above) represent a significant short-lived climate driver that can affect the Earth's radiative budget. +In addition to long-lived climate drivers such as CO2, aerosol particles represent a significant short-lived climate driver that can affect the Earth's radiative budget  (Figure 1)
 Aerosols can either directly scatter or absorb sunlight, or act as cloud nuclei, thereby influencing the Earth's radiative balance.  Aerosols can either directly scatter or absorb sunlight, or act as cloud nuclei, thereby influencing the Earth's radiative balance. 
 +They can arise from spray, technical, and biological sources (Figure 2),
 +and also volcanic eruptions (Figure 3).
 To gain a deeper understanding of how human activities have influenced the Earth's climate and how future climate change may unfold in the context of reduced human emissions, it is essential to have a basic grasp of the aerosol climate effect.  To gain a deeper understanding of how human activities have influenced the Earth's climate and how future climate change may unfold in the context of reduced human emissions, it is essential to have a basic grasp of the aerosol climate effect. 
 However, this understanding is complex.  However, this understanding is complex. 
 Aerosols can both warm and cool the Earth's climate Aerosols can both warm and cool the Earth's climate
-due to they impact on the shortwave and longwave radiation budget (cf. figure right). +due to they impact on the shortwave and longwave radiation budget (cf. Figure 1). 
  
 This presentation will provide a fundamental understanding of the effect of aerosols on the Earth's climate and present the latest results obtained using a wide range of methods employed in aerosol and climate research. This presentation will provide a fundamental understanding of the effect of aerosols on the Earth's climate and present the latest results obtained using a wide range of methods employed in aerosol and climate research.
 +
 +<wrap lo center>
 +{{ :en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker:smog-painting.png?nolink |}}
 +
 +**Figure 3.**  William Turner's painting “Fighting Temeraire” from 1838, shortly after the Tambora eruption in 1815.
 +Source:  see page 10 in  [[#ref1|[3]]].
 +</wrap>
 +
 </WRAP> </WRAP>
 <WRAP half column> <WRAP half column>
 +
 <wrap lo center> <wrap lo center>
 {{ :en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker:earth-radiation.png?nolink |}} {{ :en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker:earth-radiation.png?nolink |}}
  
-Contribution of (top) shortwave and (bottom) longwave radiation to the Earth's radiative balance.  +**Figure 1.**  Contribution of (top) shortwave and (bottom) longwave radiation to the Earth's radiative balance.  
-Source: Panels (a) and (b) of Fig 7.7 of [2].+Source: Panels (a) and (b) of Fig 7.7 of [[#ref1|[1]]]. 
 +</wrap> 
 + 
 +<wrap lo center> 
 +{{  .:2025-01-16_poehlker:aerosol-particles-bw.png?nolink  |}} 
 + 
 +**Figure 2.** Exemplary illustrations of atmospheric particles and bioaerosols. Source:  Fig. 1 of  [[#ref1|[2]]].
 </wrap> </wrap>
 </WRAP> </WRAP>
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-{{ :en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker:smog-painting.png?nolink&400 |}} 
  
  
 ==== Literature ==== ==== Literature ====
  
-   Janine Fröhlich-Nowoisky, Christopher J. Kampf, Bettina Weber, J. Alex Huffman, Christopher Pöhlker, Meinrat O. Andreae, Naama Lang-Yona, Susannah M. Burrows, Sachin S. Gunthe, Wolfgang Elbert, Hang Su, Peter Hoor, Eckhard Thines, Thorsten Hoffmann, Viviane R. Després, Ulrich Pöschl: **Bioaerosols in the Earth system: Climate, health, and ecosystem interactions.** [[https://doi.org/10.1016/j.atmosres.2016.07.018|Atmospheric Research 182 (2016) 346-376]]. +   <wrap #ref1 /O. Boucher, D. Randall, P. Artaxo, C. Bretherton, G. Feingold, P. Forster, V.-M. Kerminen, Y. Kondo, H. Liao, U. Lohmann, P. Rasch, S.K. Satheesh, S. Sherwood, B. Stevens and X.Y. Zhang:  [[https://www.ipcc.ch/site/assets/uploads/2018/02/WG1AR5_Chapter07_FINAL-1.pdf|Clouds and Aerosols.]] In: **Climate Change 2013: The Physical Science Basis.** Contribution of Working Group I to the [[https://www.ipcc.ch/assessment-report/ar5/|Fifth Assessment Report of the Intergovernmental Panel on Climate Change]] [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press 2013, Cambridge, United Kingdom and New York, NY, USA. 
-   O. Boucher, D. Randall, P. Artaxo, C. Bretherton, G. Feingold, P. Forster, V.-M. Kerminen, Y. Kondo, H. Liao, U. Lohmann, P. Rasch, S.K. Satheesh, S. Sherwood, B. Stevens and X.Y. Zhang: [[https://www.ipcc.ch/site/assets/uploads/2018/02/WG1AR5_Chapter07_FINAL-1.pdf|Clouds and Aerosols.]] In: **Climate Change 2013: The Physical Science Basis.** Contribution of Working Group I to the [[https://www.ipcc.ch/assessment-report/ar5/|Fifth Assessment Report of the Intergovernmental Panel on Climate Change]] [Stocker, T.F., D. Qin, G.-K. Plattner, M. Tignor, S.K. Allen, J. Boschung, A. Nauels, Y. Xia, V. Bex and P.M. Midgley (eds.)]. Cambridge University Press 2013, Cambridge, United Kingdom and New York, NY, USA. +   -  <wrap #ref2 />  Janine Fröhlich-Nowoisky, Christopher J. Kampf, Bettina Weber, J. Alex Huffman, Christopher Pöhlker, Meinrat O. Andreae, Naama Lang-Yona, Susannah M. Burrows, Sachin S. Gunthe, Wolfgang Elbert, Hang Su, Peter Hoor, Eckhard Thines, Thorsten Hoffmann, Viviane R. Després, Ulrich Pöschl: **Bioaerosols in the Earth system: Climate, health, and ecosystem interactions.** [[https://doi.org/10.1016/j.atmosres.2016.07.018|Atmospheric Research 182 (2016) 346-376]]. 
 +    <wrap #ref3 />  S. Brönnimann, D. Krämer:  **Tambora and the “Year Without a Summer” of 1816. A Perspective on Earth and Human Systems Science.**  [[https://doi.org/10.4480/GB2016.G90.01|Geographica Bernensia G90 (2016)]].
  
 ---- ----
-Talk  on  16January 2024 — [[.:start|Ringvorlesung in Winter Term 2024/25]]+Talk  on  16 January 2025 — [[.:start|Ringvorlesung in Winter Term 2024/25]] 
 + 
 +~~DISCUSSION|Discussion and Feedback~~
en/bne/ringvorlesung_wise2024-25/2025-01-16_poehlker.1720286939.txt.gz · Last modified: 2024/07/06 19:28 by Jürgen Vollmer