AEMET-
γ
SREPS
Convection-permitting LAM-EPS
VI Simposio Nacional de Predicción 17/19
th-September 2018
Servicios centrales AEMET
Outline
•
Who are we ?
AEMET predictability group
•
What is
AEMET-
γ
SREPS
?
20-membersnon-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
•
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., andcollaborations 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: SPPTPau Escribà
Assimilation LETKF
Mauri Martínez
(CLARITY project)
γ
SREPS support and verificationMarc Compte
(scholarship)
γ
SREPS supportJesús Rodríguez
(EUMETNET SRNWPEPSII project) calibration
David Gil
(collaboration) web pageDavid Quintero
machine learning
and
γ
SREPS support•
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”
What is
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
AEROgeneratorsSerra De Burgo (Orense)
Valladolid 2011-05-30 Hailstorm
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
•
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 ?
Designing
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
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
NWP models’ settings
HARMONIEs
WRF-ARW
NMMB
AROME
physics
ALARO
physics
65 Hybrid
sigma-pressure
verticallevels
60 s
time stepARW
dynamical core
66 72 sigma (ETA)
hydrostatic-pressure levels
up
to 40 hPa [
where it is 64 HARMONIE vertical level]
12 s
time stepNMM
dynamical core
66 72 Hybrid
sigma-pressure
up to 40 hPa
5.625 s
time stepLambert Conformal Conic projection:
lon -2.5º / lat 40.0º centre565 * 469
grid-points
Rotated lon-lat B-grid:
lon -2.5º / lat 40.0º centre
568 * 472
grid-points Calling radiation every 15 minutes8 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
•
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
γ
SREPS
Objective
VERIFICATION
AEMET-
γ
SREPSis always the better LAM-EPS !!!
•
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 !!!
γ
SREPS
Subjective
VERIFICATION
Not significant conclusions … based on
only few cases !!! See
Pau Escribà
presentation
Qualitative verification results
Stratiform precipitation
Maresme
case study:
low predictability
HARMONIE 40
HARMONIE 38
γ
SREPS PROB > 5mm
γ
SREPS max AccPcp
AEMET-
γ
SREPS
Current and future
γ
SREPS
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
]
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
]
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 profiles – Probabilistic 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
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