Each sample groups how it was prepared, characterized, and measured. Click a card to expand.
Simulated graphene aerosol particles used in Mars warming plume-tracking experiments; the study uses a bimodal disk distribution to cover thermal-IR windows.
No measurements recorded
CStudied Material
Simulated aluminum aerosol particles used in Mars warming plume-tracking experiments; modeled as rods in the atmospheric transport simulations.
No measurements recorded
AlStudied Material
Materials
graphene
C
Studied Material
Also known as
carbongraphene disks
Variables
particle_shape= disk
studied material
Paper details
Research paper
Computational MultiscaleTheoretical
Atmospheric dynamics of IR-active particles released from Mars' surface
Mark I. Richardson, Samaneh Ansari, Bowen Fan, Ramses Ramirez et al.
Each sample groups how it was prepared, characterized, and measured. Click a card to expand.
Simulated graphene aerosol particles used in Mars warming plume-tracking experiments; the study uses a bimodal disk distribution to cover thermal-IR windows.
No measurements recorded
CStudied Material
Simulated aluminum aerosol particles used in Mars warming plume-tracking experiments; modeled as rods in the atmospheric transport simulations.
No measurements recorded
AlStudied Material
Materials
graphene
C
Studied Material
Also known as
carbongraphene disks
Variables
particle_shape= disk
studied material
Paper details
Research paper
Computational MultiscaleTheoretical
Atmospheric dynamics of IR-active particles released from Mars' surface
Mark I. Richardson, Samaneh Ansari, Bowen Fan, Ramses Ramirez et al.
Each sample groups how it was prepared, characterized, and measured. Click a card to expand.
Simulated graphene aerosol particles used in Mars warming plume-tracking experiments; the study uses a bimodal disk distribution to cover thermal-IR windows.
No measurements recorded
CStudied Material
Simulated aluminum aerosol particles used in Mars warming plume-tracking experiments; modeled as rods in the atmospheric transport simulations.
No measurements recorded
AlStudied Material
Materials
graphene
C
Studied Material
Also known as
carbongraphene disks
Variables
particle_shape= disk
studied material
Paper details
Research paper
Computational MultiscaleTheoretical
Atmospheric dynamics of IR-active particles released from Mars' surface
Mark I. Richardson, Samaneh Ansari, Bowen Fan, Ramses Ramirez et al.
Each sample groups how it was prepared, characterized, and measured. Click a card to expand.
Simulated graphene aerosol particles used in Mars warming plume-tracking experiments; the study uses a bimodal disk distribution to cover thermal-IR windows.
No measurements recorded
CStudied Material
Simulated aluminum aerosol particles used in Mars warming plume-tracking experiments; modeled as rods in the atmospheric transport simulations.
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
1D radiative-convective equilibrium model with Mars-average insolation used as a cross-check on warming.custom model
Settings
insolationMars-average
model family1D radiative-convective equilibrium
comparison rolecross-check
Samples:
Other Computational
Single Column Model version of WRF used as a cross-check on warming.WRF SCM
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
1D radiative-convective equilibrium model with Mars-average insolation used as a cross-check on warming.custom model
Settings
insolationMars-average
model family1D radiative-convective equilibrium
comparison rolecross-check
Samples:
Other Computational
Single Column Model version of WRF used as a cross-check on warming.WRF SCM
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
1D radiative-convective equilibrium model with Mars-average insolation used as a cross-check on warming.custom model
Settings
insolationMars-average
model family1D radiative-convective equilibrium
comparison rolecross-check
Samples:
Other Computational
Single Column Model version of WRF used as a cross-check on warming.WRF SCM
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
Plume-tracking MarsWRF global atmospheric model with radiatively active engineered nanoparticle tracking; continuous near-surface release, dry atmosphere, no coagulation, no re-lofting, natural dust background prescribed, dry deposition included, gravitational settling from analytical free-molecular calculations.MarsWRF
Settings
modelMarsWRF
validation{"quantities":["background dust vertical distribution"],"references":["Montabone et al. 2015","Kleinböhl et al. 2024"],"techniques":["dust optical depth climatology"],"sourcetype":"literatureexperimentaldata"}
Other Computational
1D radiative-convective equilibrium model with Mars-average insolation used as a cross-check on warming.custom model
Settings
insolationMars-average
model family1D radiative-convective equilibrium
comparison rolecross-check
Samples:
Other Computational
Single Column Model version of WRF used as a cross-check on warming.WRF SCM
