Comparisons of Ice Cloud Parameters Obtained by Combined Remote Sensor Retrievals and Direct Methods

Sergey Y. Matrosov Cooperative Institute for Research in Environmental Sciences, University of Colorado/NOAA, Boulder, Colorado

Search for other papers by Sergey Y. Matrosov in
Current site
Google Scholar
PubMed
Close
,
Andrew J. Heymsfield National Center for Atmospheric Research, Boulder, Colorado

Search for other papers by Andrew J. Heymsfield in
Current site
Google Scholar
PubMed
Close
,
Robert A. Kropfli NOAA/Environmental Technology Laboratory, Boulder, Colorado

Search for other papers by Robert A. Kropfli in
Current site
Google Scholar
PubMed
Close
,
Brooks E. Martner NOAA/Environmental Technology Laboratory, Boulder, Colorado

Search for other papers by Brooks E. Martner in
Current site
Google Scholar
PubMed
Close
,
Roger F. Reinking NOAA/Environmental Technology Laboratory, Boulder, Colorado

Search for other papers by Roger F. Reinking in
Current site
Google Scholar
PubMed
Close
,
Jack B. Snider Cooperative Institute for Research in Environmental Sciences, University of Colorado/NOAA, Boulder, Colorado

Search for other papers by Jack B. Snider in
Current site
Google Scholar
PubMed
Close
,
Paivi Piironen University of Wisconsin—Madison, Madison, Wisconsin

Search for other papers by Paivi Piironen in
Current site
Google Scholar
PubMed
Close
, and
Edwin W. Eloranta University of Wisconsin—Madison, Madison, Wisconsin

Search for other papers by Edwin W. Eloranta in
Current site
Google Scholar
PubMed
Close
Restricted access

Abstract

Ice cloud microphysical parameters derived from a remote sensing method that uses ground-based measurements from the Environmental Technology Laboratory’s Ka-band radar and an IR radiometer are compared to those obtained from aircraft sampling for the cirrus priority event from the FIRE-II experiment. Aircraft cloud samples were taken not only by traditional two-dimensional probes but also by using a new video sampler to account for small particles. The cloud parameter comparisons were made for time intervals when aircraft were passing approximately above ground-based instruments that were pointed vertically. Comparing characteristic particle sizes expressed in terms of median mass diameters of equal-volume spheres yielded a relative standard deviation of about 30%. The corresponding standard deviation for the cloud ice water content comparisons was about 55%. Such an agreement is considered good given uncertainties of both direct and remote approaches and several orders of magnitude in natural variability of ice cloud parameters. Values of reflectivity measured by the radar and calculated from aircraft samples also showed a reasonable agreement; however, calculated reflectivities averaged approximately 2 dB smaller than those measured. The possible reasons for this small bias are discussed. Ground-based and aircraft-derived particle characteristic sizes are compared to those available from published satellite measurements of this parameter for the cirrus priority case from FIRE-II. Finally, simultaneous and collocated, ground-based measurements of visible (0.523 nm) and longwave IR (10–11.4 μm) ice cloud extinction optical thickness obtained during the 1995 Arizona Program are also compared. These comparisons, performed for different cloud conditions, revealed a relative standard deviation of less than 20%;however, no systematic excess of visible extinction over IR extinction was observed in the considered experimental events.

Corresponding author address: Dr. Sergey Y. Matrosov, NOAA/ERL/ETL, R/E/ET6, 325 Broadway, Boulder, CO 80303.

Abstract

Ice cloud microphysical parameters derived from a remote sensing method that uses ground-based measurements from the Environmental Technology Laboratory’s Ka-band radar and an IR radiometer are compared to those obtained from aircraft sampling for the cirrus priority event from the FIRE-II experiment. Aircraft cloud samples were taken not only by traditional two-dimensional probes but also by using a new video sampler to account for small particles. The cloud parameter comparisons were made for time intervals when aircraft were passing approximately above ground-based instruments that were pointed vertically. Comparing characteristic particle sizes expressed in terms of median mass diameters of equal-volume spheres yielded a relative standard deviation of about 30%. The corresponding standard deviation for the cloud ice water content comparisons was about 55%. Such an agreement is considered good given uncertainties of both direct and remote approaches and several orders of magnitude in natural variability of ice cloud parameters. Values of reflectivity measured by the radar and calculated from aircraft samples also showed a reasonable agreement; however, calculated reflectivities averaged approximately 2 dB smaller than those measured. The possible reasons for this small bias are discussed. Ground-based and aircraft-derived particle characteristic sizes are compared to those available from published satellite measurements of this parameter for the cirrus priority case from FIRE-II. Finally, simultaneous and collocated, ground-based measurements of visible (0.523 nm) and longwave IR (10–11.4 μm) ice cloud extinction optical thickness obtained during the 1995 Arizona Program are also compared. These comparisons, performed for different cloud conditions, revealed a relative standard deviation of less than 20%;however, no systematic excess of visible extinction over IR extinction was observed in the considered experimental events.

Corresponding author address: Dr. Sergey Y. Matrosov, NOAA/ERL/ETL, R/E/ET6, 325 Broadway, Boulder, CO 80303.

Save
  • Atlas, D., M. Kerker, and W. Hitschfeld, 1953: Scattering and attenuation by non-spherical atmospheric particles. J. Atmos. Terr. Phys.,3, 108–119.

    • Crossref
    • Export Citation
  • Brown, P. R. A., and P. N. Francis, 1995: Improved measurements of ice water content in cirrus using a total-water probe. J. Atmos. Oceanic Technol.,12, 410–414.

    • Crossref
    • Export Citation
  • ——, A. J. Illingworth, A. J. Heymsfield, G. M. McFarquhar, K. A. Browning, and M. Gosset, 1995: The role of spaceborne millimeter-wave radar in the global monitoring of ice cloud. J. Appl. Meteor.,34, 2346–2366.

    • Crossref
    • Export Citation
  • Dowling, D. R., and L. F. Radke, 1990: A summary of the physical properties of cirrus clouds. J. Appl. Meteor.,29, 970–987.

    • Crossref
    • Export Citation
  • Heymsfield, A. J., 1977: Precipitation development in stratiform ice clouds: A microphysical and dynamical study. J. Atmos. Sci.,34, 367–381.

    • Crossref
    • Export Citation
  • ——, and G. M. McFarquhar, 1996: High albedos of cirrus in the tropical Pacific warm pool: Microphysical interpretations from CEPEX and from Kwajalein, Marshall Islands. J. Atmos. Sci.,53, 2424–2450.

    • Crossref
    • Export Citation
  • ——, K. M. Miller, and J. D. Spinhirne, 1990: The 27–28 October 1986 FIRE IFO cirrus case study: Cloud microstructure. Mon. Wea. Rev.,118, 2313–2328.

    • Crossref
    • Export Citation
  • Klimowski, B. A., 1995: The 1995 Arizona Program. Field Operation Plan, The University of Arizona, 67 pp. [Available from Department of Atmospheric Sciences, The University of Arizona, Tucson, AZ 85721.].

  • Kosarev, A. L., and I. P. Mazin, 1989: Empirical model of physical structure of the upper level clouds of the middle latitude. Radiation Properties of Cirrus Clouds, E. M. Feigelson, Ed., Nauka, 29–52.

  • Liao, L., and K. Sassen, 1994: Investigation of relationships between Ka-band radar reflectivity and ice and liquid water content. Atmos. Res.,34, 231–248.

    • Crossref
    • Export Citation
  • Matrosov, S. Y., 1993: Possibilities of cirrus particle sizing from dual- frequency radar measurements. J. Geophys. Res.,98, 20675–20683.

    • Crossref
    • Export Citation
  • ——, 1997: Variability of microphysical parameters in high-altitude ice clouds: Results of the remote sensing method. J. Appl. Meteor.,36, 633–648.

    • Crossref
    • Export Citation
  • ——, T. Uttal, J. B. Snider, and R. A. Kropfli, 1992: Estimation of ice cloud parameters from ground-based infrared radiometer and radar measurements. J. Geophys. Res.,97, 1567–1574.

    • Crossref
    • Export Citation
  • ——, B. W. Orr, R. A. Kropfli, and J. B. Snider, 1994: Retrieval of vertical profiles of cirrus cloud microphysical parameters from Doppler radar and infrared radiometer measurements. J. Appl. Meteor.,33, 617–626.

    • Crossref
    • Export Citation
  • ——, A. J. Heymsfield, J. M. Intrieri, B. W. Orr, and J. B. Snider, 1995: Ground-based remote sensing of cloud particle sizes during the 26 November 1991 FIRE-II cirrus case: Comparisons with in situ data. J. Atmos. Sci.,52, 4128–4142.

    • Crossref
    • Export Citation
  • McFarquhar, G. M., and A. J. Heymsfield, 1996: Microphysical characteristics of three anvils sampled during the Central Equatorial Pacific experiment. J. Atmos. Sci.,53, 2401–2423.

    • Crossref
    • Export Citation
  • Minnis, P., K. N. Liou, and Y. Takano, 1993: Inference of cirrus cloud properties using satellite-observed visible and infrared radiances. Part I: Parameterization of radiance fields. J. Atmos. Sci.,50, 1279–1304.

  • Mitchell, D. L., 1996: Use of mass- and area-dimensional power laws for determining precipitation particle terminal velocities. J. Atmos. Sci.,53, 1710–1723.

    • Crossref
    • Export Citation
  • Ou, S. C., and Coauthors, 1995: Remote sounding of cirrus cloud optical depth and ice crystal sizes from AVHHR data: Verification using FIRE II IFO measurements. J. Atmos. Sci.,52, 4143–4158.

    • Crossref
    • Export Citation
  • Piironen, P., and E. W. Eloranta, 1994: Demonstration of a high spectral resolution lidar based on an iodine absorption filter. Opt. Lett.,19, 234–236.

    • Crossref
    • Export Citation
  • Platt, C. M. R., and A. C. Dilley, 1979: Remote sensing of high clouds. Part II: Emissivity of cirrostratus. J. Appl. Meteor.,18, 1144–1150.

  • Randall, D. A., 1995: Atlantic Stratocumulus Transition Experiment. J. Atmos. Sci.,52, 2705–2706.

    • Crossref
    • Export Citation
  • Sassen, K., 1987: Ice cloud content from radar reflectivity. J. Climate Appl. Meteor.,26, 1050–1053.

    • Crossref
    • Export Citation
  • ——, 1990: Is there a cirrus small particle radiative anomaly? Preprints, Conf. on Cloud Physics, San Francisco, CA, Amer. Meteor. Soc., J91–J95.

  • Stamnes, K., S-C. Tsay, W. Wiscombe, and K. Jayaweera, 1988: Numerically stable algorithm for discrete-ordinate method radiative transfer in multiple scattering and emitting layered media. Appl. Opt.,27, 2502–2509.

    • Crossref
    • Export Citation
  • Starr, D. O’C., and D. P. Wylie, 1990: The 27–28 October 1986 FIRE cirrus case study: Meteorology and clouds. Mon. Wea. Rev.,118, 2259–2287.

    • Crossref
    • Export Citation
  • Stephens, G. L., 1995: First ISCCP Regional Experiment Intensive Field Operations II. J. Atmos. Sci.,52, 4041–4042.

    • Crossref
    • Export Citation
  • Stokes, G. M., and S. E. Schwartz, 1994: The atmospheric radiation measurement (ARM) program: Programmatic background and design of the cloud and radiation test bed. Bull. Amer. Meteor. Soc.,75, 1201–1221.

    • Crossref
    • Export Citation
All Time Past Year Past 30 Days
Abstract Views 0 0 0
Full Text Views 944 709 73
PDF Downloads 75 26 2