the Convection-Permitting Model at JMA Tadashi Fujita, Yoshihiro - - PowerPoint PPT Presentation

the convection permitting model at jma
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the Convection-Permitting Model at JMA Tadashi Fujita, Yoshihiro - - PowerPoint PPT Presentation

Development of the Operational Data Assimilation System for Rapid and Frequent Updates of Forecast with the Convection-Permitting Model at JMA Tadashi Fujita, Yoshihiro Ishikawa, Yasutaka Ikuta, Kosuke Ono, Kensuke Ishii, Koichi Yoshimoto,


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Development of the Operational Data Assimilation System for Rapid and Frequent Updates of Forecast with the Convection-Permitting Model at JMA

Tadashi Fujita, Yoshihiro Ishikawa, Yasutaka Ikuta, Kosuke Ono, Kensuke Ishii, Koichi Yoshimoto, Junichi Ishida, Tabito Hara, Kohei Kawano, Haruka Kurahashi, Kengo Matsubayashi, Nobumiki Kinoshita, Takumu Egawa, Yuki Kosaka and Hisaki Eito

Numerical Prediction Division, Japan Meteorological Agency

6th WMO Symposium on Data Assimilation 1

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SLIDE 2

Local NWP System (LA + LFM)

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  • Objectives: providing information for aviation weather forecast and

disaster prevention, with emphasis on forecasting severe events

  • High resolution NWP: Grid spacing of 2km (the finest in the JMA’s
  • perational NWP system)
  • High frequency operation: 24 times a day (hourly)
  • In operation from Aug. 2012

Domain 1581 x 1301 covering the whole Japan

Local NWP System Local Forecast Model (LFM) Local Analysis (LA) Global NWP System Global Spectral Model (GSM) Global Analysis (GA) Meso-Scale NWP System Meso-Scale Model(MSM) Meso-Scale Analysis (MA)

Resolution ~20km Resolution 5km Resolution 2km

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SLIDE 3

6th WMO Symposium on Data Assimilation 3

Local NWP System (LA + LFM)

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SLIDE 4

4

  • High resolution

– Explicit representation of spatial and temporal variations at fine scale – More realistic terrain help resolve terrain induced phenomena mitigate representativeness error in use of surface observations

  • High frequency

– Frequently provide an enhanced forecast with information from the latest observations. – Hourly operation of rapid forecasts using an efficient system.

Features of the Local NWP System

4

Meso(5km)

6th WMO Symposium on Data Assimilation

Local(2km)

High mountains and valleys are more realistically resolved.

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SLIDE 5

14 Jul. 2012 01UTC 1-hour accumulated precipitation

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LFM predicts two line shaped heavy precipitation areas. High resolution helps better representing the strong vertical transportation of convection.

  • bservation

Features of the Local NWP System High Resolution

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SLIDE 6

Time(UTC)

00 03 06 09 12 15 18 21 00 Da12 Da18 Da00 Da06 Ea00 Ef00 Ea06 Ef06 Ea12 Ef12 Ea18 Ef18 Ma00 Mf00 Ma03 Mf03 Ma06 Mf06 Ma09 Mf09 Ma12 Mf12 Ma15 Mf15 Ma18 Mf18 Ma21 Mf21

La 00 Lf 00 La 01 Lf 01 La 02 Lf 02 La 03 Lf 03 La 04 Lf 04 La 05 Lf 05 La 06 Lf 06 La 07 Lf 07 La 08 Lf 08 La 09 Lf 09 La 10 Lf 10 La 11 Lf 11 La 12 Lf 12 La 13 Lf 13 La 14 Lf 14 La 15 Lf 15 La 16 Lf 16 La 17 Lf 17 La 18 Lf 18 La 19 Lf 19 La 20 Lf 20 La 21 Lf 21 La 22 Lf 22 La 23 Lf 23

Global Mesoscale Local

6th WMO Symposium on Data Assimilation 6

~20km 2km 5km

Local NWP System:High Frequency Operation

  • Hourly update of forecasts initialized using the

latest observations.

  • LFM Results become available by initial time +70
  • min. (compared to +150min for MSM)

Features of the Local NWP System High Frequency Operation

Da: Global Cycle Analysis Ea: Global Early Analysis Ef: Global Forecast Ma:Mesoscale Analysis Mf: Mesoscale Forecast La: Local Analysis Lf:Local Forecast

Long cutoff-time: keeping quality of the entire system. Short cutoff-time: keeping distribution of products on schedule.

4D-Var 4D-Var 4D-Var 3D-Var

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SLIDE 7

6th WMO Symposium on Data Assimilation 7

FT=9

470min 410min

FT=8

350min

FT=7 FT=7 FT=9

390min

FT=6

290min

FT=5

230min

FT=6

210min

FT=4

170min

FT=3

110min

FT=2

50min

Updates of Forecasts valid at 7/11 18UTC from different initial times (1h accumulated precipitation)

  • bservation

Lead Time LFM MSM

Features of the Local NWP System High Frequency Operation

3 hourly updates. Results available by Initial time +150min. Frequent updates reflecting newly received observations. Results available by initial time + 70min.

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SLIDE 8

6th WMO Symposium on Data Assimilation

LA system

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  • assimilate the latest observations through 3h analysis cycle (iterate

3D-Var + 1-hour forecasts)

  • use MSM forecast (initialized with 4D-Var) as the first guess
  • Data Cut off time: 30 minutes, Resolution: 5km, 50 vertical levels

3h before LFM initial time

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SLIDE 9

6th WMO Symposium on Data Assimilation 9

LA system

Observations Assimilated to Initialize JMA Operational Forecast Models

G: Global Analysis, M: Meso-scale Analysis, L: Local Analysis ( ) : under development for introduction

  • LA makes extensive use of

surface observations.

  • Remote sensing data are used

as important sources of detailed information for forecasting high impact events. ・Development is in progress for introduction of satellite data (Brightness Temperature and Atmospheric Motion Vector).

Extensive use of data with high temporal resolution (rapid scan satellite data, etc.) is considered to be an important challenge in the future.

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SLIDE 10

6th WMO Symposium on Data Assimilation

Ground-based GNSS

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LA system: Distribution of Assimilated Observation Data

Aviation Surface

(AMeDAS, SYNOP, SHIP, DRIFTER)

Doppler radar Radar reflectivity Wind Profiler TEMP, PILOT

30 Sep. 2013 00UTC

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SLIDE 11

LA system

Use of radar reflectivity observation

MSM LF1 3DVAR Radar simulator Radar obs. Ze RH pseudo obs. Ze-RH Database

without Radar Ze with Radar Ze OBSERVATION Estimated RH PDF for different values of Ze

Altitude 3000m Ze RH

Kernel Density Estimation of PDF + Maximum Likelihood Estimation

  • Y. Ikuta, 2012: CAS/JSC

WGNE Res. Activ. Atmos. Oceanic Modell., 42, 01.05-01.06.

3h accumulated precipitation 27 Jul. 2011, 18UTC

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Ongoing Development: enhancement of LA cycle

FT=3 FT=3 FT=2 FT=2 FT=1 FT=1 Observation Operational System Test System

2km

Incremental approach

2km 5km 5km

Updates of 1h accumulated Precipitation Forecasts (all valid at 06 Jul. 2012 11UTC from different initial times) new forecast

  • ld forecast

LFM LA LFM LA

Test to enhance resolution

  • f the last 1h forecast.

Operational Test Contribute to improve spin-up of precipitation forecast, mitigating shock from different resolutions.

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SLIDE 13

asuca (NL,TL,AD) Physics Library (NL,TL,AD)

  • Obs. operator

(NL,TL,AD) External packages (NL,TL,AD) ex.: RTTOV 3D-Var 4D-Var +Hybrid asuca-Var core

Selector switch is implemented Interface for each observed element Wrapper for each package asuca-Var core is specialized to handle optimization and related processes

asuca-3DVar applied to the Local NWP

Test system asuca-Var + asuca(5km) => asuca(2km) Operational system JNoVA + JMA-NHM(5km)=> JMA-NHM(2km)

Observation

Ongoing Development: asuca-Var

JMA has started to develop a new framework of forecast and analysis systems.

  • rganized design and coordinated development of

Non-linear, Tangent-linear and Adjoint codes

Physics Library: a repository of various physical process routines with unified specification asuca-Var : Variational data assimilation system based on “asuca” asuca: new dynamical core

Forecast comparable to the operational one

1h precipitation 11 Jul. 2012, 22UTC

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SLIDE 14

Ongoing Development Use of Satellite Brightness Temperature Data

GPS TPW MTSAT-2 Clear Sky Radiance

MTSAT-2 contributes to greatly increase humidity information

  • ver the sea.

Example of MTSTAT-2 Jacobian

dTb/dqv dTb/dT

altitude (km)

MTSAT-2 GPS

Altitude 8000m

Increment /

bg sat v v

q q

asuca-3DVar Assimilation Experiment

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SLIDE 15

6th WMO Symposium on Data Assimilation 15

Summary

The Local NWP is the finest resolution system in the JMA’s operational NWP system, aimed at providing information on aviation forecast and disaster prevention. The convection-permitting resolution of LFM allows enhanced prediction of high impact events. The system is featured with high frequency and rapid updates of forecasts using the latest observations. Use of radar obs. etc. contributes to a better forecast of high impact events. Various developments are in progress to improve the Local NWP system. These includes:

  • enhancement of the LA cycle (high resolution 1h-forecast in the last part of the

cycle), contributing to improve spin-up of precipitation forecast.

  • development of a new framework of forecast and analysis systems (asuca and

asuca-Var), achieving a comparable performance with the current operational Local NWP system.

  • introduction of satellite observations (TB, AMV), contributing to greatly increase
  • bservation coverage.