Nephelometer Measurements of the Asymmetry Parameter, Volume Extinction Coefficient, and Backscatter Ratio in Arctic Clouds

By H. Gerber, Y. Takano, Timothy J. Garrett, P. Hobbs. 2000

139 citations recorded by the source corpus.

Subfields: Aerospace Engineering, Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/651cd109a8d4788c19e8dd4f83f1fdc98ceab0f0

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Aerospace Engineering

1. Alexander Marshak
2. C. Schmitt
3. David D. Turner
4. Ping Yang
5. S. A. Clough
6. Anthony J. Baran
7. Bryan A. Baum
8. Andrew J. Heymsfield

In Atmospheric Science

1. Ping Yang
2. Anthony J. Baran
3. Bryan A. Baum
4. David D. Turner
5. C. Schmitt
6. Alexander Marshak
7. Andrew J. Heymsfield
8. Zhien Wang

In Global and Planetary Change

1. Ping Yang
2. Anthony J. Baran
3. Bryan A. Baum
4. David D. Turner
5. C. Schmitt
6. Alexander Marshak
7. Andrew J. Heymsfield
8. Zhien Wang

Citations in the corpus

• Effective Ice Particle Densities Derived from Aircraft Data (2004, background): “Instruments that accurately measure IWCs are now be- coming available (e.g., counterflow virtual impactor, Twohy et al. 1997), and re can be derived together with coincident direct measurements of the extinction (Gerber et al. 2000).”
• Thin Liquid Water Clouds: Their Importance and Our Challenge (2007, background): “Examples of such instruments include an airborne transmissometer (Korolev et al. 1999), a cloud extinctometer (Zmarzly and Lawson 2000), a cloud-integrating nephelometer ( Gerber et al. 2000 ), and an in situ lidar (Evans et al. 2003, 2006).”
• A review of the light scattering properties of cirrus (2009, methodology): “There have been attempts to ‘‘measure’’ g most notably using the Cloud Integrating Nephelometer (CIN) described in [132].”
• Representation of a nonspherical ice particle by a collection of independent spheres for scattering and absorption of radiation: 2. Hexagonal columns and plates (2003, methodology): “For complex ice crystals with concavities, measurements in Arctic clouds [Gerber et al., 2000] have found an average gx of 0.74. Since gs 0.87 for the equal-V/A spheres, we would expect the altered t in the model to compensate for the altered g, yielding R 1 if F 2. Schmitt and Heymsfield [2005] hav”
• Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part II: Narrowband Models (2005, methodology): “Taken with other cirrus observations by Auriol et al. (2001) and Gerber et al. (2000), g ranges from 0.73 to 0.78.”