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The added value of scatterometer ocean surface wind for the limited area model HARMONIE

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The added value of scatterometer ocean surface wind for the limited area model HARMONIE in extreme weather events Gert-Jan Marseille KNMI – The Netherlands [email protected]. Motivation. EU-funded MyWave project (mywave.eu) - PowerPoint PPT Presentation
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1(of 11) EMS - Reading - 10/9/2013 The added value of scatterometer ocean surface wind for the limited area model HARMONIE in extreme weather events Gert-Jan Marseille KNMI – The Netherlands [email protected]
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Page 1: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

1(of 11)EMS - Reading - 10/9/2013

The added value of scatterometer ocean surface wind

for the limited area model HARMONIE in extreme weather events

Gert-Jan MarseilleKNMI – The Netherlands

[email protected]

Page 2: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

2(of 11)EMS - Reading - 10/9/2013

Motivation

• EU-funded MyWave project (mywave.eu)• What is the additional value of scatterometer (SCAT) ocean surface winds for

ocean wave and storm surge forecasting?– Verification– Direct assimilation of SCAT winds in wave/surge models– Indirect: model wind (with assimilated SCAT) used as input for wave/surge models

• Focus on extreme weather events– 2006/10/28 – 2006/11/03 - NW-W storm. "The storm is marked as a surge- and

SWL record in Delfzijl and well known as Allerheiligenvloed or the “Horses storm”, because 227 horses were isolated due to flood in Marrum, 25 horses drowned, the rest was saved in a spectacular rescue operation.“

– 2007/11/05 - 2007/11/11 - NW storm. "The first storm since the building of the Nieuwe Waterweg and the Maeslantkering that was closed due to the exceeding the threshold water levels in Hoek van Holland“

– 2011/07/11 – 2011/07/17 - NE storm. Not very common but interesting, one of the periods used in the assessment of the operational SWAN model for the North Sea.

– 2011/12/06 – 2012/01/06 - A 1 month period that includes Ulli (Rapid development over UK 2012-01-03 Storm Ulli).

Page 3: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

3(of 11)EMS - Reading - 10/9/2013

Satellite Scatterometers

ASCAT

www.knmi.nl/scatterometer

In this study we use:• ASCAT (METOP-A)• QuikSCAT• Oceansat-2

• Ocean surface wind speed and direction

• global coverage

• Increasing spatial and temporal resolution

Page 4: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

4(of 11)EMS - Reading - 10/9/2013

• Non-hydrostatic

• 800x800 grid

• 2.5 km grid size

• 3D-var assimilatie– 4/8 times per day

– 36-hour forecast

• ECMWF boundaries

• Available since 1/1/2012

Harmonie model(Hirlam ALADIN Research on Meso-scale Operational NWP in Euromed)

Page 5: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

5(of 11)EMS - Reading - 10/9/2013

Scatterometer assimilation in Harmonie

• Works technically!• First experiments in Harmonie using ASCAT and

QuikSCAT18:52

18:52

20:22

20:22

Harmonie DA default settings• 6-hour assimilation window; too large

for fast moving weather systems

• Scatterometer usage based on ECMWF SCAT usage

• ASCAT thinning: factor 4 in both directions => ~94% not used

• QSCAT: no thinning

AN: 18UTCQuikSCAT

TEMP, AIREP, SYNOP, ASCAT, SCAT locations

Page 6: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

6(of 11)EMS - Reading - 10/9/2013

Analysis increment

• Red circles: analysis increment mainly from assimilation of scatterometer

• Scatterometer corrects model winds in the order of a couple of ms-1

Model 10-m wind+

assimilated ASCAT

model 10-manalysis increment

Page 7: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

7(of 11)EMS - Reading - 10/9/2013

Learning how to use observations in Harmonie DA

• Four experiments to address questions like– What does data assimilation add to HARMONIE forecast improvement?– What is the optimal assimilation window length: 6/3/1/… hour?– What is the optimal density/weight given to observations?– Apply averaging or thinning of dense observations (Mode-S/radar

wind/SCAT/…)?– How well is quality control?

1. NoDA: No data assimilation2. Conv: Assimilation of conventional observations

(TEMP/Aircraft/SYNOP) only3. Conv + ASCAT/QSCAT (default settings)4. Conv + ASCAT – no thinning

Page 8: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

8(of 11)EMS - Reading - 10/9/2013

Case study: closure Maeslantkering

• Part of the Dutch Delta Works plan (initiated after the 1953 flooding disaster) to protect the South-Western part of the Netherlands for high sea levels

• Closed for the first time:– 9 November 2007

Page 9: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

9(of 11)EMS - Reading - 10/9/2013

surface wind speed

AN: 2007110900FC+6

VT: 2007110906

ECMWF underestimates

wind overNorth Sea

121110987

654321

no assim ECMWF

Closure Maeslantkering

verifying qscat

assim: conv + ascat + qscat

Page 10: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

10(of 11)EMS - Reading - 10/9/2013

surface wind speed

AN: 2007110900FC+6

VT: 2007110906

Note the maximumwind speed in

South-West Netherlands for

conv+scat experiment

121110987

654321

no assim

conv + ascat + qscat

ECMWF

verifying qscat

Closure Maeslantkering… zooming in to The Netherlands

Page 11: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

11(of 11)EMS - Reading - 10/9/2013

Harmonie DA• Does improve analysis• does not improve

250hPa-T forecast• does improve 850hPa-

T forecast

• does not improve 850hPa-u/v forecast

• Scat impact on model wind at 850 hPa, not at 250hPa (deviation green/blue/cyan)

Forecast verification using aircraft observations

No assimConvConv+ascat+qscatConv+ascat – no thinnECMWF

Page 12: The added value of scatterometer  ocean surface wind  for the limited area model HARMONIE

12(of 11)EMS - Reading - 10/9/2013

Status and plans

• Status– Analyzing the results from the experiments– First conclusion: added value of DA in HARMONIE is a bit disappointing

based on standard bias/RMSE scores but some issues encountered:• Too large weight is given to observations• QC not strict enough; poor quality observations are still accepted for

DA

• Plans– Recommendations on how to optimally use observations in HARMONIE

(weights, thinning, averaging, quality control, …..)– Make HARMONIE ready for the assimilation of the Indian scatterometer

Oceansat-2– Run the other selected cases– Disseminate HARMONIE model fields to project partners as input for

wave/surge models.


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