real time nowcasting in the western us or why you can’t use nodes c0-2

42
Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2 George Thomas Andy Wood Dennis Lettenmaier Department of Civil and Environmental Engineering LAND SURFACE HYDROLOGY RESEARCH GROUP Group Seminar July 5, 2006

Upload: kadeem-cooke

Post on 03-Jan-2016

37 views

Category:

Documents


0 download

DESCRIPTION

Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2. George Thomas Andy Wood Dennis Lettenmaier Department of Civil and Environmental Engineering LAND SURFACE HYDROLOGY RESEARCH GROUP Group Seminar July 5, 2006. Outline. Objective background surface water monitor - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Real Time Nowcasting In The Western UsOR

Why you can’t use nodes C0-2

George ThomasAndy Wood

Dennis Lettenmaier

Department of Civil and Environmental Engineering

LAND SURFACE HYDROLOGY RESEARCH GROUPGroup Seminar

July 5, 2006

Page 2: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Outline

Objective

background surface water monitor westwide forecast system challenges

index station method for real-time forcing generation

implementation details

progress / results to date

future plans

Page 3: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Objective

Monitor the hydrologic state of the US land surface Initially, western US; soon, mexico + remainder of US 1/8 degree Daily updates in real-time (lag of 12-36 hrs) Soil moisture, snow, runoff Fully automated Consistent with retrospective: back to at least 1950

Can be used for hazard assessment Drought Flood risk

Can be used to initialize hydrologic forecasts Short lead, 1-15 day Long lead, 1-12 month

Page 4: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background

This nowcast draws upon procedures and data from two existing systems assembled by Dr. Wood

UW Experimental Surface Water Monitor (1/2 degree) Methods for real-time forcing generation & model

updating

UW West-wide Seasonal Hydrologic Forecasting System VIC model data at 1/8 degree Eventually, forecast methods

The nowcast will eventually be an integral part of the West-wide forecasting system

Page 5: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

SW Monitor Background

An outgrowth of the west-wide forecasting system that adds a national scale perspective on land surface moisture

directly relevant to retrospective drought reconstruction work going on in our group Andreadis et al. (2005) paper on drought ½ degree VIC input parameters

enabled by recent NCDC extension of digital data archives back to 1915

will be used as platform for drought and hydrologic analyses in real-time

nowcasts are used now by US Drought Monitor & US Drought Outlook authors (at CPC and elsewhere)

many products possible, such as following one:

Page 6: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Drought Severity and Spatial Extent

Page 7: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Monitor Webpage

dailyupdates

1-2 day lag

soil moisture& SWEpercentiles

½ degreeresolution

archive from1915-current

uses ~2130index stns

Page 8: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: UW SW Monitor

trends:1 week2 week1 month

Archive!

Page 9: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: UW SW Monitor

Archive from 1915-current

current conditions are a productof the same simulation (samemethods, ~same stations) ashistorical conditions

allows comparison of current conditions with historical ones

can navigate by month or year

People: Andy, Ali, Kaiyuan, Dennis

Page 10: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: UW SW Monitor

Page 11: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: West-wide Forecasting System

Soil MoistureInitial

Condition

SnowpackInitial Condition

Page 12: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: West-wide Forecasting System

NEW: West-wide overview of flow forecasts

(mouse-over/clickablefor more details)

Page 13: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

As previously, flow location maps give access to monthly hydrograph plots, and also to data.

Background: West-wide Forecasting System

Now clicking the stream flow forecast map also accesses current basin-averaged conditions

Page 14: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

An earlier G. Thomas contribution:

Automating plots of west-wide SWE data

Background

West-wide Forecasting System

Daily UpdatingWest-at-a-glanceSWE fromNRCS, EC, CADWR

Analyses: Current Anomalies Percentiles:

Current1-week change2-week change

Page 15: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Background: Central Challenge

Model simulations are calibrated and validated using a uniform or consistent set of forcing data

Nowcasts and forecasts use models calibrated and validated retrospectively

Problem: the station data used to create forcings are not as widely available in real-time as they are for the retrospective calibration/validation period

Solution: the “index-station method”

# st

atio

ns

time 3 monthsbefore present

present

Page 16: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

VIC model spinup methods: index stationsestimating spin-up period inputs

dense station network for model calibration sparse station network in real-time

Page 17: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Outline

Objective

background surface water monitor westwide forecast system challenges

index station method for real-time forcing generation

implementation details

progress / results to date

future plans

Page 18: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Index station method: example for precipitation

uses time-varying precipitation signal ONLY FROM stations that report reliably in real-time and for over 45 years (many go back longer)

precipitation percentiles calculated from raw precip for time period no shorter than 21 days.

percentiles interpolated to 1/8 degree grid at 1/8 degree, percentiles used to extract corresponding

observed value from 1/8 degree restrospective distribution (based on dense observing network, standard VIC forcing methods)

period 1/8 degree precip amount disaggregated using the fractional daily precipitation for that period (interpolated to 1/8 degree grid).

temperature is treated differently – daily interpolated anomalies for Tmin & Tmax are used

Page 19: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Index station method: example for precipitation

Index stn pcp (mm) pcp

percentile

gridded to 1/8 degree

1/8 degree dense station monthly pcp DISTRIBUTION(N years for each 1/8 degree grid cell)(MM)

1/8 degree pcp (mm) disagg. to

dailyusing interpolated daily fractions from index stations

monthly daily

Page 20: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Index station method: example for precipitation

In real-time, with daily updates, this method actively updates the forcings for a period from 3 weeks to 7 weeks.

case 1: current day is less than day 21 of month

treated as 1 period for percentile calculation

months

case 2: current day is greater than day 20 of month

treated as 2 periods for percentile calculation

the first month becomes fixed in forcing data

months

Page 21: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Index stationmethod

test of method for streamflow

Page 22: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Outline

Objective

background surface water monitor westwide forecast system challenges

index station method for real-time forcing generation

implementation details

progress / results to date

future plans

Page 23: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Nowcast Information Flow

VIC Retrospective SimulationDaily, 1915 to Near Current

VIC Real-timeSimulation

(~1 month long)

HydrologicState

NOAA ACIS / OtherPrcp Tmax Tmin

Coop Stations

Index Station Method Gridded Forcing Creation

Hydrologic values, anom’s, %-iles w.r.t.retrospective PDF

climatology (PDF)of

hydrologic valuesw.r.t. defined period

vals, anoms%-iles

w.r.t. PDF

1955+

HydrologicState

(-1 Day)

1930s

Page 24: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Computing Environment: Flood Cluster 46 cores9 AMD Opteron 2x dual core2 Intel Xeon 2X single core1 AMD Opteron 2x single core

Rocks 4.0.0 / CentOS 4.0 Linux

Nowcasting is implemented on nodes c0-2 and c0-6

Useful phrases: WTF?! (what the flood?!)

RTFM!! (read the flood manual)

Page 25: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

SW Monitor coding scheme

downloadobs

P, tx, tn

update

force

VIC

Station

Index filesclimatology

Forcings

2 mon

Params

Soil, etc.

output

Page 26: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

SW Monitor coding scheme – NCAST implementation

downloadobs

P, tx, tn

update

force

VIC

Station

Index filesclimatology

Forcings

2 mon

Params

Soil, etc.

output

obs

P, tx, tn

update

force

VIC

output

Forcings

2 mon

Params

Soil, etc.

climatology Station

Index files

Node 0-2 Node 0-6

Loop over basinsca, colo, gbas, riog

Loop over basinspnw, mexn, mexs

Page 27: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

Page 28: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

1. ACIS for CONUS2123 stations1915-present

Page 29: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

1. ACIS for CONUS2123 stations1915-present

2. Environment Canada10 stations1915-present

Page 30: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

1. ACIS for CONUS2123 stations1915-present

2. Environment Canada10 stations1915-present

Page 31: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

1. ACIS for CONUS2123 stations1915-present

2. Environment Canada10 stations1915-present

3. Mexico (retrospective)739 stations1925-2003

Page 32: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Implementation Details

Observation data:Real-time and retrospectivestations.3 Primary sources

1. ACIS for CONUS2123 stations1915-present

2. Environment Canada10 stations1915-present

3. Mexico (retrospective)739 stations1925-2003Real-Time: EDAS (Eta DAS) daily re-analysis

Page 33: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Outline

Objective

background surface water monitor westwide forecast system challenges

index station method for real-time forcing generation

implementation details

progress / results to date

future plans

Page 34: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

daily forecast of SM percentiles

Page 35: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

daily forecast of SM percentiles – animations of recent forecasts

Page 36: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

daily forecast of SM percentiles - comparison with SW Monitor

Page 37: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

daily forecast of SM percentiles - comparison with CPC Drought Monitor

Page 38: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

daily forecast of SM percentiles - 2 week change - comparison with SW Monitor

Page 39: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Results

April 1 SWE Archive(1997 – 2006)

Page 40: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Outline

Objective

background surface water monitor westwide forecast system challenges

index station method for real-time forcing generation

implementation details

progress / results to date

future plans

Page 41: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

Future Work

Ongoing and Future Work data products expansion (Arkansas, etc.) routing constraints using SWE

Page 42: Real Time Nowcasting In The Western Us OR Why you can’t use nodes C0-2

END

Thank you!