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AEMET-γSREPS: convection-permitting LAM-EPS [Presentación]

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(1)

AEMET-

γ

SREPS

Convection-permitting LAM-EPS

VI Simposio Nacional de Predicción 17/19

th

-September 2018

Servicios centrales AEMET

(2)

Outline

Who are we ?

AEMET predictability group

What is

AEMET-

γ

SREPS

?

20-members

non-hydrostatic convection-permitting

EPS

Designing

AEMET-

γ

SREPS

Multi-boundary conditions + multi-mesoscale NWP models

γ

SREPS

in operations

EcFlow suite gSREPSoper

γ

SREPS

verification

Subjective and objective

Current and future

γ

SREPS

developments

(3)
(4)

Since 2002 an small core group working on Limited Area

(LAM) Ensemble Prediction

Systems

(EPS) depending on Research Deparment

Members of

HIRLAM

-GLAMEPS-HarmonEPS and involved in several projects:

EUMETNET SRNWP EPS II, PreFlexMS, COASTEPS, EPS eCOST action, etc., and

collaborations on EPSs with

IPMA

-AEMET, AROME-EPS

MétéoFrance

, etc.

AEMET-

γ

SREPS Predictability group

José Antonio García-Moya

(retired on May 2018)

BCsand experiments on all aspects of EPS

Alfons Callado

γ

SREPS operational development and model error: SPPT

Pau Escribà

Assimilation LETKF

Mauri Martínez

(CLARITY project)

γ

SREPS support and verification

Marc Compte

(scholarship)

γ

SREPS support

Jesús Rodríguez

(EUMETNET SRNWPEPSII project) calibration

David Gil

(collaboration) web page

David Quintero

machine learning

and

γ

SREPS support

(5)

Full participation in

VI Simposio Nacional de Predicción

: 5 presentations

AEMET-

γ

SREPS in other presentations:

• El episodio de Oliva-Gandía del 3-4 noviembre de 1987: récord nacional de precipitación en 24 horas (C. Santos et al.) • Episodio de cizalladura del 10-9-2017 en el aeropuerto de Barcelona (A. Méndez et al.)

Coastal trapped disturbancesen el litoral catalán: un peligro aeronáutico (S. González et al.)

• Episodio de tiempo severo con elevado impacto en Cataluña del 18 de octubre de 2017 (R. Pascual and G. Cuevas)

AEMET-

γ

SREPS Predictability group

José Antonio García-Moya

Super-CHAIRMAN

Alfons Callado

“AEMET-

γ

SREPS: convection permitting LAM-EPS”

Pau Escribà

“El

AEMET-γSREPS en un caso de convección por convergencias en el Mediterráneo”

Mauri Martínez

“nowcRadiation – Software de nowcasting para la predicción de la radiación solar”

David Gil

“Presentación de la aplicación web AEMET-

γ

SREPS”

David Quintero

“Postproceso estadístico de modelos meteorológicos

con Machine Learning: aplicaciones al γSREPS y al HARMONIE”

(6)

What is

(7)

Turia 1957-10-14 Flash flood>350mm/d

La Safor 2007--Cut-off low>450mm/d CVal 2009-09-27/29 Cut-off low>300mm/d Cádiz 2009-12-24 Tornado Algeciras 2012-03-06 Storm > 35 mm/h

Montserrat 2000-06-09 Flash-floods > 200mm

Vista Alegre 1999-09-07 Tornado

Tous 1982-10-20 Flash-floods>1000mm Cantábrico 2011-05-30

CAP gale (Galerna)

Spain

Severe

Weather

Spain

Renewable

Energies

AEROgenerators

Serra De Burgo (Orense)

Valladolid 2011-05-30 Hailstorm

(8)

AEMET-

γ

SREPS system

NMMB WRF ARW

HARMONIE-ALARO

HARMONIE-AROME Multi-BCs

Multi-NWP

CMC / GEM JMA / GSM

MF / ARPÈGE NCEP / GFS

ECMWF / IFS

We are now updating

WRF-ARW from 3.6.0 on

sigma levels to 3.9.1.1 on

hybrid !!!

20-members

non-hydrostatic convection-permitting

EPS

Since April 2016 daily running at

00

and

12 UTC

up to

36 hours

(9)

Multi-model

HARMONIE-AROME

HARMONIE-ALARO

WRF-ARW (NCAR)

NMMB (NCEP)

AEMET-

γ

SREPS

1

INITIAL

CONDITIONS

HH+00

HH+24

HH+48

X X

X

X

K

P

P

D

t

X

Initial conditions

and

Multi-BCs

ECMWF – IFS

NCEP – GFS

MétéoFrance – ARPÈGE

CMC – GEM (Canadian)

JMA - GSM (Japanese)

2

BOUNDARY

CONDITIONS

3

MODEL

ERROR

Developing a

convection-permitting

LAM-EPS

3 sources of uncertainties

2019

LETKF

assimilation

25 members

¿ GEM-LAM ?

(10)

Designing

(11)

Horizontal resolution in

GRIB

files

HARMONIEs

lambert

‘NLON' => '576’,

'NLAT' => '480',

‘EZONE’ => ’11’

'GSIZE' => '2500.',

WRF-ARW

map_proj = ‘lambert',

e_we = 566,

e_sn = 470,

dx = 2500,

dy = 2500,

NMMB

map_proj = 'rotated_llb',

e_we = 568,

e_sn = 472,

dx = 0.022545,

dy = 0.022500,

NMMB bigger area than HARMONIE to interpolate to common

Lambert area without missing values

Intended to

run each NWP

with the same /

very

similar

internal

GRID

Exactly

the

(12)

Vertical levels consistence

between models

AROME

and

ALARO

65

hybrid

sigma-pressure

layers

No top

WRF-ARW

:

72

sigma levels

hybrid on

3.9.1. version

Top 40 hPa

NMMB

72

hybrid levels

Top 40 hPa

Consistency AT LOW LEVELS into the

PBL

The very close vertical levels

distribution !!!

22

(13)

NWP models’ settings

HARMONIEs

WRF-ARW

NMMB

AROME

physics

ALARO

physics

65 Hybrid

sigma-pressure

vertical

levels

60 s

time step

ARW

dynamical core

66 72 sigma (ETA)

hydrostatic-pressure levels

up

to 40 hPa [

where it is 64 HARMONIE vertical level

]

12 s

time step

NMM

dynamical core

66 72 Hybrid

sigma-pressure

up to 40 hPa

5.625 s

time step

Lambert Conformal Conic projection:

lon -2.5º / lat 40.0º centre

565 * 469

grid-points

Rotated lon-lat B-grid:

lon -2.5º / lat 40.0º centre

568 * 472

grid-points Calling radiation every 15 minutes

8 LBC relaxation points around grid area

Summary of models in

γ

SREPS:

4

NWP MODELS

It has been intended to integrate both NWP models with the closer possible settings in order to be the comparison the more fairly possible.

X

(14)
(15)

EcFlow

suite management

00 and 12 UTC cycle over

IBERIA_2.5

domain

Downloading

NCEP / GFS

BCs

20

members

EPS

γ

SREPS at

ECMWF

Cray XC40

Running

NMMB

+

NCEP/GFS BCs

UPP

NCEP Unified Post-processor

HARMONIE

AROME

+

ECMWF/IFS BCs

HARMONIE

ALARO

+

ECMWF/IFS BCs

Finishing !!!

Cray XC40 ECMWF

(16)

γ

SREPS

Objective

VERIFICATION

AEMET-

γ

SREPS

is always the better LAM-EPS !!!

(17)

AEMET-

γ

SREPS

without assimilation

HARMONIE-LETKF

As HarmonEPS, but with LETKF

HARMONIE-3DVAR-EPS

HarmonEPS

3DVAR-NMC + EC-SLAF

HARMONIE-3DVAR-LAG

8 mbrs det. HARMONIE

AEMET-

γ

SREPS

is always the better LAM-EPS !!!

(18)

γ

SREPS

Subjective

VERIFICATION

Not significant conclusions … based on

only few cases !!! See

Pau Escribà

presentation

(19)

Qualitative verification results

Stratiform precipitation

(20)

Maresme

case study:

low predictability

HARMONIE 40

HARMONIE 38

γ

SREPS PROB > 5mm

γ

SREPS max AccPcp

AEMET-

γ

SREPS

(21)

Current and future

γ

SREPS

(22)

Foreseeable future work

plan: 2018-2020

γ

SREPS

“scientific” developments:

Assimilation:

LETKF

without discarding

3DVAR…

[

Pau

]

• GNSS+

RADAR

assimilation [

Jana Sánchez

]

• 25 members

Including the 5th

mesoscale

convection-permitting

NWP model:

¿Canadian

GEM-LAM

? [

Alfons

]

(23)

Foreseeable future work

plan: 2018-2020

γ

SREPS

“technical” developments:

γ

SREPS

IBERIA

at

ECMWF

systems:

• Time critical application

level 2 [

Pau

]

• IBERIAxxm_2.5

bigger domain (~better organized

convection) and up to

72 hours

2020 Bologna

HPCF supercomputer

γ

SREPS

CANARIAS_2.5

00 and 12 UTC at

AEMET

systems (

BULL-ATOS

):

• Currently under implementation [

Alfons

+

David Q.

]

• ¿ “explotación” future mamagement ? [

Sergio Cotera

]

(24)

Foreseeable future work

plan: 2018-2020

γ

SREPS

user “products” developments:

Probabilistic forecast products:

• Forecasters

WEB page

[

David G.,

see presentation

]

With one click:

EPSgrams

Probabilistic vertical profilesProbabilistic cross-sections

PANEL-VIM

integration [

ATAP Marcos G.

]

Specific socio-economic

impact

products:

AEROgrams

ENAIRE

[

Mariona Pons

&

Alejandro Méndez

]

¿

Wind shear

products ?

Wind

/

solar

renewable energy sector:

E.g. probabilistic solar

GHI

+

DNI

for

REE

[¿

Mauri

?]

Barcelona airport

(25)

Happy AEMET-γSREPSing !!!

[email protected]

[email protected]

AEMET

-

γ

SREPS will be shortly available for AEMET forecasters !!!

For your case studies, ask for AEMET-

γ

SREPS !!!

VI Simposio Nacional de Predicción 17/19

th

-September 2018

Servicios centrales AEMET

AEMET Predictability Group

Referencias

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