PACJET Projects |
HMT 2004
PACJET 2003
PACJET 2002
PACJET 2001
CALJET 1998
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Publications |
Snow Level Detection (pdf)
Orographic Precipitation (pdf)
ETL S-band Radar (pdf)
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Data |
GWINDEX
West Coast RUC
ETL Profiler Network
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Background |
About Pacjet
CALJET Summary
Societal Impacts and User Input
Linkages to National Priorities
USWRP
Data Assimilation Implementation Plan
NSSL Briefing
Press Release
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Programs Documents |
PACJET 2001 and a
Long-term Effort to Improve 0-24h West Coast Forecasts
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PACJET Community |
NOAA Research:
ETL,
NSSL,
FSL
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National Weather Service Western Region:
Eureka,
Hanford,
Medford,
Monterey,
Oxnard,
Portland,
Reno,
Sacramento,
San Diego,
Seattle,
CNRRC,
NWRFC
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Office of Marine and Aviation Operations:
AOC
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Naval Postgradute School
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DRI CIASTA
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CIRES
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SUNY Stony Brook
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National Centers for Environmental Prediction:
EMC,
HPC,
MPC
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National Environmental Satellite, Data
and Information Service
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CIMSS
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CIRA
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Operational Forecasting Components |
COMET Precipitation
Presentation
West Coast RUC
Aircraft Obs via AWIPS
GWINDEX Poster
Applications Development
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Research Components |
Modeling Research Components
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Related Experiments |
Winter Storm Reconnaissance (Central Pac.)
IMPROVE (Microphysics)
THORPEX (Synoptic Targeting)
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Observing Systems |
NOAA P-3
Wind Profiler Network
Satellite Products
NOAA S-band Radar
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Contact |
Marty Ralph
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Planning Workshops |
2001 - Monterey, CA
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OAR Hot Items Bulletin
Orographic precipitation enhancement
- rain rate is most strongly controlled by upslope winds at 1 km altitude, especially in a LLJ
- blocking increases rain upstream of terrain
- precipitation efficiency is 50% higher when a LLJ is present than when it is not:
0.9 (mm h-1) (m s-1)-1 with a LLJ vs. 0.6 (mm h-1) (m s-1)-1 without a LLJ
Warm rain
- rain rates in west coast storms can exceed 20 mm/h in conditions without a bright band
- for cases with the same rain rate, reflectivities were roughly 8 dBZ lower in warm rain cases
- 35% of rain in the 1997/98 winter occurred without a bright band, < 5% did in 2000/01
- Significant rain can occur without a bright band, but not every year.
Bright-band detection
- an automated algorithm using wind profiler observations was developed and is being tested
- real time output are on the web and deduced altitudes are a better estimate of snow level than is the 0°C level
- rapid 2000 ft increases in melting level are often observed and can triple runoff in CA watersheds
Sea-surface fluxes and coastal rainfall
- high surface winds combined with anomalously warm coast SSTs can increase coastal rain
- observations in a flooding event showed a 27% increase in CAPE due to these fluxes
- this flooding event was capped off by convective rain rates that reached 80 mm/h
Flooding in adjacent watersheds
- wind direction in the warm sector of a major storm determined the location of a rainshadow
- the rain shadow resided partially over one watershed but not over an adjacent watershed
- small (± 10°) wind direction variations can strongly affect winter flooding in complex terrain
Narrow moisture plumes
- P-3 soundings offshore with roughly 80 km spacing documented a narrow moisture plume
- the core of the plume was roughly 100 km wide, with IWV > 3.0 cm
- the core values were 40% greater than the maximum IWV derived from GOES due to clouds
- Key aspects of a narrow moist plume responsible for a 4" rain event were missed by GOES and numerical models.
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