An annual cycle of Arctic cloud characteristics observed by radar and lidar at SHEBA

By J. Intrieri, Matthew Shupe, T. Uttal, B. McCarty. 2002

385 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/99de2d94dc544b6044011e094f4a1683207fc53c

How researchers see this paper

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

In Atmospheric Science

1. Hugh Morrison
2. Ulrike Lohmann
3. Matthew Shupe
4. M. Krämer
5. S. Abel
6. James Pinto
7. A. Korolev
8. Paul R. Field

In Global and Planetary Change

1. Hugh Morrison
2. Ulrike Lohmann
3. Matthew Shupe
4. M. Krämer
5. S. Abel
6. Paul R. Field
7. M. Schnaiter
8. J. Crosier

Citations in the corpus

• Arctic Mixed-Phase Cloud Properties from AERI Lidar Observations: Algorithm and Results from SHEBA (2005, methodology): “*Standard ARM retrieval (Liljegren and Lesht 1996), which uses monthly retrieval coefficients developed from the Liebe and Layton (1987) absorption model for dry air and water vapor and the Grant et al.”
• Mesoscale modeling of springtime Arctic mixed-phase stratiform clouds using a new two-moment bulk microphysics scheme (2005, methodology): “…and mean Doppler velocity up to a height of 13 km. Collocated with the MMCR were a dual-channel microwave radiometer (MWR) and a depolarization micropulse lidar used to remotely determine liquid water path (LWP), cloud phase, and cloudbase height (Westwater et al. 2001; Intrieri et al. 2002).”
• A ground‐based multisensor cloud phase classifier (2007, background): “Cloud liquid is identified by high lidar backscatter and low depolarization ratio [e.g., Sassen, 1984; Intrieri et al., 2002], as are present in both the low-level cloud layer and at the top of the mid-level cloud near 4 km in Figures 1a and 1b. High backscatter is due to the high total surface…”
• Mixed-Phase Clouds: Progress and Challenges (2017, background): “Jackson et al. (2012) found that, in Arctic clouds, liquid droplet concentrations were well correlated with aerosol concentrations below cloud, whereas ice crystal number concentrations were better correlated with aerosol concentrations above cloud.”
• ‘Application of a New Spectral Theory of Stably Stratified Turbulence to the Atmospheric Boundary Layer over Sea Ice’ (2005, background): “During the Surface Heat Budget of the Arctic Ocean (SHEBA) experiment, clear-sky conditions were observed 27% of the time (Intrieri et al., 2002).”
• Aerosol number–size distributions during clear and fog periods in the summer high Arctic: 1991, 1996 and 2001 (2006, background): “In the summer Arctic, on the other hand, low stratus clouds and fogs are very frequent (Huschke, 1969; Curry, 1986; Intrieri et al., 2002).”