[PDF][PDF] Deconvolution of Boundary Layer Depth and Aerosol Constraints on Cloud Water Path in Subtropical Stratocumuli
The liquid water path (LW P) adjustment due to aerosol-cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …
Deconvolution of boundary layer depth and aerosol constraints on cloud water path in subtropical stratocumulus decks
The liquid water path (LWP) adjustment due to aerosol–cloud interactions in marine
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …
stratocumulus remains a considerable source of uncertainty for climate sensitivity estimates …
[PDF][PDF] Precipitation Susceptibility of Marine Stratocumulus with Variable Above and Below-Cloud Aerosol Concentrations over the Southeast Atlantic.
1 https://doi. org/10.5194/acp-2021-677 Preprint. Discussion started: 9 September 2021 cс
Author (s) 2021. CC BY 4.0 License. to separated profiles. In clean boundary layers (below …
Author (s) 2021. CC BY 4.0 License. to separated profiles. In clean boundary layers (below …
Magnitude and timescale of liquid water path adjustments to cloud droplet number concentration perturbations for nocturnal non-precipitating marine stratocumulus
Cloud liquid water path (L) adjusts to perturbations in cloud droplet number concentration
(N) over time. We explore the magnitude and timescale of this adjustment in nocturnal non …
(N) over time. We explore the magnitude and timescale of this adjustment in nocturnal non …
How Cloud Droplet Number Concentration Impacts Liquid Water Path and Precipitation in Marine Stratocumulus Clouds—A Satellite-Based Analysis Using …
Aerosol–cloud–precipitation interactions (ACI) are a known major cause of uncertainties in
simulations of the future climate. An improved understanding of the in-cloud processes …
simulations of the future climate. An improved understanding of the in-cloud processes …
Aerosol indirect effects in marine stratocumulus: The importance of explicitly predicting cloud droplet activation
I Bulatovic, AML Ekman, J Savre… - Geophysical …, 2019 - Wiley Online Library
Climate models generally simulate a unidirectional, positive liquid water path (LWP)
response to increasing aerosol number concentration. However, satellite observations and …
response to increasing aerosol number concentration. However, satellite observations and …
[PDF][PDF] Does precipitation susceptibility vary with increasing cloud thickness in marine stratocumulus?
The relationship between precipitation rate and accumulation mode aerosol concentration in
marine stratocumulus-topped boundary layers is investigated by applying the precipitation …
marine stratocumulus-topped boundary layers is investigated by applying the precipitation …
Diurnal patterns in the observed cloud liquid water path response to droplet number perturbations
KM Smalley, MD Lebsock… - Geophysical Research …, 2024 - Wiley Online Library
A key uncertainty in Aerosol‐cloud interactions is the cloud liquid water path (LWP)
response to increased aerosols (λ). LWP can either increase due to precipitation …
response to increased aerosols (λ). LWP can either increase due to precipitation …
Does precipitation susceptibility vary with increasing cloud thickness in marine stratocumulus?
The relationship between precipitation rate and accumulation mode aerosol concentration in
marine stratocumulus-topped boundary layers is investigated by applying the precipitation …
marine stratocumulus-topped boundary layers is investigated by applying the precipitation …
Precipitation susceptibility in marine stratocumulus and shallow cumulus from airborne measurements
Precipitation tends to decrease as aerosol concentration increases in warm marine
boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this …
boundary layer clouds at fixed liquid water path (LWP). The quantitative nature of this …