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contributor authorCocks, Stephen B.
contributor authorMartinaitis, Steven M.
contributor authorKaney, Brian
contributor authorZhang, Jian
contributor authorHoward, Kenneth
date accessioned2017-06-09T17:16:41Z
date available2017-06-09T17:16:41Z
date copyright2016/03/01
date issued2015
identifier issn1525-755X
identifier otherams-82286.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225383
description abstractrecently implemented operational quantitative precipitation estimation (QPE) product, the Multi-Radar Multi-Sensor (MRMS) radar-only QPE (Q3RAD), mosaicked dual-polarization QPE, and National Centers for Environmental Prediction (NCEP) stage II QPE were evaluated for nine cool season precipitation events east of the Rockies. These automated, radar-only products were compared with the forecaster quality-controlled NCEP stage IV product, which was considered as the benchmark for QPE. Community Collaborative Rain, Hail and Snow Network (CoCoRaHS) 24-h accumulation data were used to evaluate product performance while hourly automated gauge data (quality controlled) were used for spatial and time series analysis. Statistical analysis indicated all three radar-only products had a distinct underestimate bias, likely due to the radar beam partially or completely overshooting the predominantly shallow winter precipitation systems. While the forecaster quality-controlled NCEP stage IV estimates had the best overall performance, Q3RAD had the next best performance, which was significant as Q3RAD is available in real time whereas NCEP stage IV estimates are not. Stage II estimates exhibited a distinct tendency to underestimate gauge totals while dual-polarization estimates exhibited significant errors related to melting layer challenges.
publisherAmerican Meteorological Society
titleMRMS QPE Performance during the 2013/14 Cool Season
typeJournal Paper
journal volume17
journal issue3
journal titleJournal of Hydrometeorology
identifier doi10.1175/JHM-D-15-0095.1
journal fristpage791
journal lastpage810
treeJournal of Hydrometeorology:;2015:;Volume( 017 ):;issue: 003
contenttypeFulltext


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