A variational technique to estimate snowfall rate from coincident radar, snowflake, and fall-speed observations

Cooper, Steven J.; Wood, Norman B.; L'Ecuyer, Tristan S.

doi:https://doi.org/10.5194/amt-10-2557-2017

Articles | Volume 10, issue 7

https://doi.org/10.5194/amt-10-2557-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/amt-10-2557-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 10, issue 7

Research article

|

20 Jul 2017

Research article |

| 20 Jul 2017

A variational technique to estimate snowfall rate from coincident radar, snowflake, and fall-speed observations

Steven J. Cooper, Norman B. Wood, and Tristan S. L'Ecuyer

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Final revised paper (published on 20 Jul 2017)
Preprint (discussion started on 15 Feb 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review of "A variational technique to estimate snowfall rate from coincident radar, snowflake, and fallspeed observations"', Anonymous Referee #1, 02 Mar 2017
- AC1: 'Author Response', Steven Cooper, 27 Apr 2017
RC2: 'Reviewer comments', Anonymous Referee #2, 23 Mar 2017
- AC2: 'Author Response', Steven Cooper, 27 Apr 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Steven Cooper on behalf of the Authors (27 Apr 2017) Author's response Manuscript

ED: Referee Nomination & Report Request started (01 May 2017) by Dominique Ruffieux

RR by Anonymous Referee #1 (18 May 2017)

RR by Anonymous Referee #2 (24 May 2017)

ED: Publish subject to minor revisions (Editor review) (08 Jun 2017) by Dominique Ruffieux

AR by Steven Cooper on behalf of the Authors (12 Jun 2017) Author's response Manuscript

ED: Publish as is (13 Jun 2017) by Dominique Ruffieux

Short summary

Estimates of snowfall rate as derived from radar observations can suffer large uncertainties due to great natural variability in snowflake microphysical properties. We used in situ observations of particle size, shape, and fall speed to refine radar-based estimates of snowfall for five snow events at the ARM Barrow Climate Research Facility. Estimated snowfall amounts agreed well with nearby snow gauge observations and demonstrated significant sensitivity to both particle shape and fall speed.