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NOAA’s National Weather Service Middle Atlantic River Forecast Center Weather Forecast Office State College Ted Rodgers Hydrometeorologist Cody Moser Hydrologist.

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Presentation on theme: "NOAA’s National Weather Service Middle Atlantic River Forecast Center Weather Forecast Office State College Ted Rodgers Hydrometeorologist Cody Moser Hydrologist."— Presentation transcript:

1 NOAA’s National Weather Service Middle Atlantic River Forecast Center Weather Forecast Office State College Ted Rodgers Hydrometeorologist Cody Moser Hydrologist

2 Weather Forecast Offices 122 WFOs

3 River Forecast Centers 13 RFCs

4 Hydro Challenges: Precip drives our rivers Access to Gulf &Atlantic Moisture Topographically enhanced precip Coastal Storms Lake effect Mixed cool season precip Ice jams Snow melt Flashy headwaters Fast responding streams (6 – 12 hrs) Densely populated – lead time critical Towns established (as early as 1600s) along the rivers Chesapeake Bay – coastal inundation, water quality Recent repetitive major flooding Political pressure to end flooding Mid-Atlantic River Basins

5 Forecast Responsibility  7 days a week including holidays  6am to 11pm  24 hrs during flooding  ~160 Daily Forecast Points  ~8 Flood-Only Forecast Points  ~300 Supplemental Points  4 daytime shifts  1 Hydrometeorologist  3 Hydrologists  1 evening shift  Flexibility in floods

6 Delaware, Passaic, Raritan Susquehanna HAS Forecaster Potomac, James, Rappahannock WFO State CollegeConference Room Mt Nittany

7 How the National Weather Service Forecasts River Stages

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10 1,467 Precipitation Gages

11 Basin average, 6 hourly resolution

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13 MPE = Multisensor Precipitation Estimator Radar and Gages info combined

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17 River Basins

18 1 st step in forecast process is determining the amount of runoff produced by precipitation in the basin.

19 ◦ Accounts for seasonal relationship of soil moisture conditions and surface moisture conditions ◦ Computes incremental surface runoff based on surface and overall soil- moisture conditions ◦ Computes what portion of the precip that does not become surface runoff enters groundwater storage.  Now that we know the runoff – we apply the unit hydrograph to compute the flow at the basin outlet.

20 Hydrograph resulting from 1 inch of runoff occurring uniformly over space and time. Shape is affected by the slope of the basin.

21  K and Lag ◦ Attenuation and timing ◦ Determined through calibration ◦ Can be variable with different flows

22 River Model (CHPS)

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24  Precipitation does not occur uniformly over space and/or time  Adjust model parameters ◦ Precipitation Amount ◦ Runoff Rate ◦ Rain/Snow ◦ Snowmelt Rate

25  6-8am – Hydrometeorologist (HAS) Function ◦ Past precipitation data collection (24 hours ending 7am) ◦ Quality Control of RADAR, MPE, gage precip/temp data ◦ Create 72-hr Quantitative Precipitation Forecast (QPF)  8am –Three Hydrologists Begin River Forecasting ◦ Briefing from HAS ◦ Quality control of streamgage data ◦ Run river model ◦ Make manual adjustments to model ◦ Coordination with Weather Offices ◦ Issue forecasts (around 10am) ◦ Monitor and update forecasts as needed

26 From the River Forecast Center to our Weather Forecast Offices

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29  Emergency Managers/Public ◦ Flood awareness and safety  Fisheries Management ◦ Wildlife ◦ Fisherman  Agriculture  Reservoir Managers ◦ Recreation ◦ Flood control  Hydropower ◦ Power generation Who uses our river forecasts?

30  Flood Outlooks  Flood Climatology  Water Supply  Precipitation  Flash Flood Guidance  Expansion into Water Resources  Customer Advisory Board What else do we do?

31 The Future in River Forecasting

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33  Free online learning modules http://www. meted.ucar

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