Effects of cirrus near the tropopause on anvil cirrus dynamics Garrett, T., et al. (2006), Effects of cirrus near the tropopause on anvil cirrus dynamics, Geophys. Res. Lett., 33, L17804, doi:10.1029/2006GL027071. Read more about Effects of cirrus near the tropopause on anvil cirrus dynamics
Convective formation of pileus cloud near the tropopause Garrett, T., et al. (2006), Convective formation of pileus cloud near the tropopause, Atmos. Chem. Phys., 6, 1185-1200, doi:10.5194/acp-6-1185-2006. Read more about Convective formation of pileus cloud near the tropopause
Simultaneous retrieval of aerosol and thin cirrus optical depths using MODIS airborne simulator data during CRYSTAL-FACE and CLAMS Roskovensky, J.K., et al. (2004), Simultaneous retrieval of aerosol and thin cirrus optical depths using MODIS airborne simulator data during CRYSTAL-FACE and CLAMS, Geophys. Res. Lett., 31, L18110, doi:10.1029/2004GL020457. Read more about Simultaneous retrieval of aerosol and thin cirrus optical depths using MODIS airborne simulator data during CRYSTAL-FACE and CLAMS
Nitric acid uptake on subtropical cirrus cloud particles Popp, P., et al. (2004), Nitric acid uptake on subtropical cirrus cloud particles, J. Geophys. Res., 109, D06302, doi:10.1029/2003JD004255. Read more about Nitric acid uptake on subtropical cirrus cloud particles
Ice Cloud Retrievals and Analysis with the Compact Scanning Submillimeter Imaging Radiometer and the Cloud Radar System during CRYSTAL FACE Evans, K.F., et al. (2005), Ice Cloud Retrievals and Analysis with the Compact Scanning Submillimeter Imaging Radiometer and the Cloud Radar System during CRYSTAL FACE, J. Appl. Meteor., 44, 839-859. Read more about Ice Cloud Retrievals and Analysis with the Compact Scanning Submillimeter Imaging Radiometer and the Cloud Radar System during CRYSTAL FACE
Evidence for the Predominance of Mid-Tropospheric Aerosols as Subtropical Anvil Cloud Nuclei Fridlind, A.M., et al. (2004), Evidence for the Predominance of Mid-Tropospheric Aerosols as Subtropical Anvil Cloud Nuclei, Science, 304, 718. Read more about Evidence for the Predominance of Mid-Tropospheric Aerosols as Subtropical Anvil Cloud Nuclei
Homogeneous Ice Nucleation in Subtropical and Tropical Convection and Its Influence on Cirrus Anvil Microphysics HEYMSFIELD, A., et al. (2005), Homogeneous Ice Nucleation in Subtropical and Tropical Convection and Its Influence on Cirrus Anvil Microphysics, J. Atmos. Sci., 62, 41-64. Read more about Homogeneous Ice Nucleation in Subtropical and Tropical Convection and Its Influence on Cirrus Anvil Microphysics
Validation and determination of ice water contentradar reflectivity relationships during CRYSTALFACE: Flight requirements for future comparisons Sayres, D., et al. (2008), Validation and determination of ice water contentradar reflectivity relationships during CRYSTALFACE: Flight requirements for future comparisons, J. Geophys. Res., 113, D05208, doi:10.1029/2007JD008847. Read more about Validation and determination of ice water contentradar reflectivity relationships during CRYSTALFACE: Flight requirements for future comparisons
Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part II: Narrowband Models Baum, B.A., et al. (2005), Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part II: Narrowband Models, J. Appl. Meteor., 44, 1896-1911, doi:10.1175/JAM2309.1. Read more about Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part II: Narrowband Models
Combining a receptor-oriented framework for tracer distributions with a cloud-resolving model to study transport in deep convective clouds: Application to the NASA CRYSTAL-FACE campaign Xueref, I., et al. (2004), Combining a receptor-oriented framework for tracer distributions with a cloud-resolving model to study transport in deep convective clouds: Application to the NASA CRYSTAL-FACE campaign, Geophys. Res. Lett., 31, L14106, doi:10.1029/2004GL019811. Read more about Combining a receptor-oriented framework for tracer distributions with a cloud-resolving model to study transport in deep convective clouds: Application to the NASA CRYSTAL-FACE campaign