Decomposing effective radiative forcing due to aerosol cloud interactions by global cloud regimes

Decomposing effective radiative forcing due to aerosol cloud interactions by global cloud regimes

Quantifying effective radiative forcing due to aerosol-cloud interactions (EERFACI) remains a largely uncertain process, and the magnitude remains unconstrained in general circulation models. Previous studies focus on the magnitude of ERFACI arising from all cloud types, or examine it in the framewo...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς:	Langton, T, Stier, P, Watson-Parris, D, Mulcahy, JP
Μορφή:	Journal article
Γλώσσα:	English
Έκδοση:	American Geophysical Union 2021

Παρόμοια τεκμήρια

Regime-based analysis of aerosol-cloud interactions
ανά: Gryspeerdt, E, κ.ά.
Έκδοση: (2012)

Quantifying cloud adjustments and the radiative forcing due to aerosol–cloud interactions in satellite observations of warm marine clouds
ανά: Douglas, A, κ.ά.
Έκδοση: (2020)

Quantifying cloud adjustments and the radiative forcing due to aerosol–cloud interactions in satellite observations of warm marine clouds
ανά: A. Douglas, κ.ά.
Έκδοση: (2020-05-01)

The hemispheric contrast in cloud microphysical properties constrains aerosol forcing
ανά: McCoy, IL, κ.ά.
Έκδοση: (2020)

The significant role of biomass burning aerosols in clouds and radiation in the South-eastern Atlantic Ocean
ανά: Che, H, κ.ά.
Έκδοση: (2020)

The CLoud–Aerosol–Radiation Interaction and Forcing: Year 2017 (CLARIFY-2017) measurement campaign
ανά: Haywood, JM, κ.ά.
Έκδοση: (2021)

Global response of parameterised convective cloud fields to anthropogenic aerosol forcing
ανά: Kipling, Z, κ.ά.
Έκδοση: (2019)

Global response of parameterised convective cloud fields to anthropogenic aerosol forcing
ανά: Kipling, Z, κ.ά.
Έκδοση: (2020)

Uncertainty in aerosol–cloud radiative forcing is driven by clean conditions
ανά: E. Gryspeerdt, κ.ά.
Έκδοση: (2023-04-01)

Spatial Aggregation of Satellite Observations Leads to an Overestimation of the Radiative Forcing due to Aerosol‐Cloud Interactions
ανά: Tom Goren, κ.ά.
Έκδοση: (2023-09-01)

Overview: The CLoud-Aerosol-Radiation Interaction and Forcing: Year-2017 (CLARIFY-2017) measurement campaign
ανά: Haywood, JM, κ.ά.
Έκδοση: (2020)

The CLoud–Aerosol–Radiation Interaction and Forcing: Year 2017 (CLARIFY-2017) measurement campaign
ανά: J. M. Haywood, κ.ά.
Έκδοση: (2021-01-01)

Cloud adjustments dominate the overall negative aerosol radiative effects of biomass burning aerosols in UKESM1 climate model simulations over the south-eastern Atlantic
ανά: Che, H, κ.ά.
Έκδοση: (2021)

Invisible ship tracks show large cloud sensitivity to aerosol
ανά: Manshausen, P, κ.ά.
Έκδοση: (2022)

Invisible ship tracks show large cloud sensitivity to aerosol
ανά: Manshausen, P, κ.ά.
Έκδοση: (2022)

Source attribution of cloud condensation nuclei and their impact on stratocumulus clouds and radiation in the south-eastern Atlantic
ανά: Che, H, κ.ά.
Έκδοση: (2022)

Satellite observations of cloud regime development: the role of aerosol processes
ανά: Gryspeerdt, E, κ.ά.
Έκδοση: (2014)

Satellite observations of cloud regime development: the role of aerosol processes
ανά: Gryspeerdt, E, κ.ά.
Έκδοση: (2013)

Satellite observations of cloud regime development: the role of aerosol processes
ανά: E. Gryspeerdt, κ.ά.
Έκδοση: (2014-02-01)

Strong control of effective radiative forcing by the spatial pattern of absorbing aerosol
ανά: Williams, AIL, κ.ά.
Έκδοση: (2022)

Variability in Biomass Burning Emissions Weakens Aerosol Forcing Due To Nonlinear Aerosol‐Cloud Interactions
ανά: Kyle B. Heyblom, κ.ά.
Έκδοση: (2023-06-01)

Separating radiative forcing by aerosol–cloud interactions and rapid cloud adjustments in the ECHAM–HAMMOZ aerosol–climate model using the method of partial radiative perturbations
ανά: J. Mülmenstädt, κ.ά.
Έκδοση: (2019-12-01)

Cloud adjustments dominate the overall negative aerosol radiative effects of biomass burning aerosols in UKESM1 climate model simulations over the south-eastern Atlantic
ανά: H. Che, κ.ά.
Έκδοση: (2021-01-01)

Impact of biomass burning aerosols on radiation, clouds, and precipitation over the Amazon: relative importance of aerosol–cloud and aerosol–radiation interactions
ανά: L. Liu, κ.ά.
Έκδοση: (2020-11-01)

Aerosol nucleation and its role for clouds and Earth's radiative forcing in the aerosol-climate model ECHAM5-HAM
ανά: Kazil, J, κ.ά.
Έκδοση: (2010)

Large uncertainty in future warming due to aerosol forcing
ανά: Watson-Parris, D, κ.ά.
Έκδοση: (2022)

Source attribution of cloud condensation nuclei and their impact on stratocumulus clouds and radiation in the south-eastern Atlantic
ανά: H. Che, κ.ά.
Έκδοση: (2022-08-01)

Brightening of the global cloud field by nitric acid and the associated radiative forcing
ανά: Makkonen, R, κ.ά.
Έκδοση: (2012)

Uncertainty in aerosol–cloud radiative forcing is driven by clean conditions
ανά: Gryspeerdt, E, κ.ά.
Έκδοση: (2023)

Technical Note: Estimating aerosol effects on cloud radiative forcing
ανά: S. J. Ghan
Έκδοση: (2013-10-01)

Sensitivities of cloud radiative effects to large-scale meteorology and aerosols from global observations
ανά: Andersen, H, κ.ά.
Έκδοση: (2023)

The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity
ανά: Neubauer, D, κ.ά.
Έκδοση: (2019)

The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity
ανά: Neubauer, D, κ.ά.
Έκδοση: (2019)

An overview of the ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) project: aerosol-cloud-radiation interactions in the Southeast Atlantic basin
ανά: Redemann, J, κ.ά.
Έκδοση: (2021)

The global aerosol–climate model ECHAM6.3–HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing, and climate sensitivity
ανά: D. Neubauer, κ.ά.
Έκδοση: (2019-08-01)

Decomposing the effective radiative forcing of anthropogenic aerosols based on CMIP6 Earth system models
ανά: A. Kalisoras, κ.ά.
Έκδοση: (2024-07-01)

Sensitivities of cloud radiative effects to large-scale meteorology and aerosols from global observations
ανά: H. Andersen, κ.ά.
Έκδοση: (2023-09-01)

Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
ανά: Regayre, LA, κ.ά.
Έκδοση: (2023)

Wet scavenging limits the detection of aerosol–cloud–precipitation interactions
ανά: Gryspeerdt, E, κ.ά.
Έκδοση: (2015)

An overview of the ORACLES (ObseRvations of Aerosols above CLouds and their intEractionS) project: aerosol–cloud–radiation interactions in the southeast Atlantic basin
ανά: J. Redemann, κ.ά.
Έκδοση: (2021-02-01)