en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker
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| en:bne:ringvorlesung_wise2024-25:2025-01-16_poehlker [2024/07/06 19:28] – draft created Jürgen Vollmer | en: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 ====== | ||
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| + | <WRAP group> | ||
| + | <WRAP half column> | ||
| ===== Mira Pöhlker | ===== Mira Pöhlker | ||
| - | > [[https:// | + | > [[https:// |
| + | > [[https:// | ||
| - | ==== 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> | ||
| - | {{ .: | ||
| - | Exemplary illustrations of atmospheric particles and bioaerosols. Fig. 1 of [1]. | + | ==== Abstract ==== |
| - | </ | + | |
| - | In addition to long-lived climate drivers such as CO2, aerosol particles | + | In addition to long-lived climate drivers such as CO2, aerosol particles represent a significant short-lived climate driver that can affect the Earth' |
| Aerosols can either directly scatter or absorb sunlight, or act as cloud nuclei, thereby influencing the Earth' | Aerosols can either directly scatter or absorb sunlight, or act as cloud nuclei, thereby influencing the Earth' | ||
| + | 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' | To gain a deeper understanding of how human activities have influenced the Earth' | ||
| However, this understanding is complex. | However, this understanding is complex. | ||
| Aerosols can both warm and cool the Earth' | Aerosols can both warm and cool the Earth' | ||
| - | 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' | This presentation will provide a fundamental understanding of the effect of aerosols on the Earth' | ||
| + | |||
| + | <wrap lo center> | ||
| + | {{ : | ||
| + | |||
| + | **Figure 3.** William Turner' | ||
| + | Source: | ||
| + | </ | ||
| + | |||
| </ | </ | ||
| <WRAP half column> | <WRAP half column> | ||
| + | |||
| <wrap lo center> | <wrap lo center> | ||
| {{ : | {{ : | ||
| - | Contribution of (top) shortwave and (bottom) longwave radiation to the Earth' | + | **Figure 1.** |
| - | Source: Panels (a) and (b) of Fig 7.7 of [2]. | + | Source: Panels (a) and (b) of Fig 7.7 of [[# |
| + | </ | ||
| + | |||
| + | <wrap lo center> | ||
| + | {{ .: | ||
| + | |||
| + | **Figure 2.** Exemplary illustrations of atmospheric particles and bioaerosols. Source: | ||
| </ | </ | ||
| </ | </ | ||
| Line 38: | Line 58: | ||
| - | {{ : | ||
| ==== Literature ==== | ==== Literature ==== | ||
| - | | + | |
| - | | + | - <wrap #ref2 /> Janine Fröhlich-Nowoisky, |
| + | | ||
| ---- | ---- | ||
| - | Talk on 16. January | + | Talk on 16 January |
| + | |||
| + | ~~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