What controls the vertical distribution of aerosol? Relationships between process sensitivity in HadGEM3–UKCA and inter-model variation from AeroCom Phase II
<p>The vertical profile of aerosol is important for its radiative effects, but weakly constrained by observations on the global scale, and highly variable among different models. To investigate the controlling factors, we investigate the effects of individual processes in one particular model...
Main Authors: | Kipling, Z, Stier, P, Johnson, C, Mann, G, Bellouin, N, Bauer, SE, Bergman, T, Chin, M, Diehl, T, Ghan, S, Iversen, T, Kirkevåg, A, Kokkola, H, Liu, X, Luo, G, van Noije, T, Pringle, K, von Salzen, K, Schulz, M, Seland, Ø, Skeie, R, Takemura, T, Tsigaridis, K, Zhang, K |
---|---|
Format: | Journal article |
Published: |
Copernicus Publications
2015
|
Similar Items
-
Aerosols at the poles: an AeroCom Phase II multi-model evaluation
by: Sand, M, et al.
Published: (2017) -
An AeroCom assessment of black carbon in Arctic snow and sea ice
by: Jiao, C, et al.
Published: (2014) -
The HadGEM2-ES implementation of CMIP5 centennial simulations
by: Jones, C, et al.
Published: (2011) -
Aerosol absorption in global models from AeroCom phase III
by: Sand, M, et al.
Published: (2021) -
The American monsoon system in HadGEM3 and UKESM1
by: García-Franco, JL, et al.
Published: (2020)