Development and Application of the Chinese Operational Hydrological Forecasting System

Similar documents
Data Assimilation of Argo Profiles in Northwest Pacific Yun LI National Marine Environmental Forecasting Center, Beijing

Application and improvement of Ensemble Optimal Interpolation on Regional Ocean Modeling System (ROMS)

Developing Coastal Ocean Forecasting Systems and Their Applications

Assimilation Impact of Physical Data on the California Coastal Ocean Circulation and Biogeochemistry

A Modeling Study on Flows in the Strait of Hormuz (SOH)

The High Resolution Global Ocean Forecasting System in the NMEFC and its Intercomparison with the GODAE OceanView IV-TT Class 4 Metrics

Storm surge forecasting and other Met Office ocean modelling

GFDL, NCEP, & SODA Upper Ocean Assimilation Systems

Development of a coastal monitoring and forecasting system at MRI/JMA

Improving the initialisation of our operational shelf-seas models

Initial Results of Altimetry Assimilation in POP2 Ocean Model

GODAE Ocean View Activities in JMA (and Japan)

The Improvement of JMA Operational Wave Models

Applications of an ensemble Kalman Filter to regional ocean modeling associated with the western boundary currents variations

The CONCEPTS Global Ice-Ocean Prediction System Establishing an Environmental Prediction Capability in Canada

Implementation of the SEEK filter in HYCOM

ECMWF: Weather and Climate Dynamical Forecasts

The ECMWF coupled data assimilation system

GAMINGRE 8/1/ of 7

Aquarius Data Release V2.0 Validation Analysis Gary Lagerloef, Aquarius Principal Investigator H. Kao, ESR And Aquarius Cal/Val Team

The Coupled Earth Reanalysis system [CERA]

Life Cycle of Convective Systems over Western Colombia

WIND EFFECTS ON CHEMICAL SPILL IN ST ANDREW BAY SYSTEM

Comparison between vertical shear mixing and surface wave-induced mixing in the global ocean

Evaluation of the sea ice forecast at DMI

How DBCP Data Contributes to Ocean Forecasting at the UK Met Office

Supplementary appendix

PREDICTION OF OIL SPILL TRAJECTORY WITH THE MMD-JMA OIL SPILL MODEL

Feature resolution in OSTIA L4 analyses. Chongyuan Mao, Emma Fiedler, Simon Good, Jennie Waters, Matthew Martin

Discussion of forcing errors in the Bay and how to deal with these using the LETKF. Assimilation with synthetic obs with realistic coverage

Ocean data assimilation systems in JMA and their representation of SST and sea ice fields

Observations assimilated

Yi Chao Jet Propulsion Laboratory California Institute of Technology & Joint Institute for Regional Earth System Science and Engineering (JIFRESSE)

BMKG Research on Air sea interaction modeling for YMC

NCODA Implementation with re-layerization

An Overview of Atmospheric Analyses and Reanalyses for Climate

OSSE OSE activities with Multivariate Ocean VariationalEstimation (MOVE)System. II:Impacts ofsalinity and TAO/TRITON.

Introduction of Korea Operational Oceanographic System (KOOS)

Name Period Part I: INVESTIGATING OCEAN CURRENTS: PLOTTING BUOY DATA

Assimilation of SST data in the FOAM ocean forecasting system

Lu, S., P. Craig, C. Wallen, Z. Liu, A. Stoddard, W. McAnnally and E. Maak. Dynamic Solutions, Knoxville, TN USACOE, Sacramento District

Ocean data assimilation for reanalysis

Sea Ice Forecast Verification in the Canadian Global Ice Ocean Prediction System

Yellow Sea Thermohaline and Acoustic Variability

Eddy and Chlorophyll-a Structure in the Kuroshio Extension Detected from Altimeter and SeaWiFS

Collaborative Proposal to Extend ONR YIP research with BRC Efforts

Convective-scale NWP for Singapore

Coastal Data Assimilation: progress and challenges in state estimation for circulation and BGC models

Performance of a 23 years TOPAZ reanalysis

Seasonal Simulaions of a coupled ice-ocean model in the Bohai Sea and North Yellow Sea

Demonstration and Comparison of of Sequential Approaches for Altimeter Data Assimilation in in HYCOM

Enhancing predictability of the Loop Current variability using Gulf of Mexico Hycom

ENSO Outlook by JMA. Hiroyuki Sugimoto. El Niño Monitoring and Prediction Group Climate Prediction Division Japan Meteorological Agency

Operational Estuarine & Coastal Forecast Systems in NOAA s. National Ocean Service

Overview of data assimilation in oceanography or how best to initialize the ocean?

Regional High Resolution Reanalysis over European North East Shelf domain

Operational Use of Scatterometer Winds at JMA

Impact of Argo, SST, and altimeter data on an eddy-resolving ocean reanalysis

O.M Smedstad 1, E.J. Metzger 2, R.A. Allard 2, R. Broome 1, D.S. Franklin 1 and A.J. Wallcraft 2. QinetiQ North America 2. Naval Research Laboratory

Shuhei Maeda Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency

CERA-SAT: A coupled reanalysis at higher resolution (WP1)

Changes in spatial distribution of chub mackerel under climate change: the case study using Japanese purse seine fisheries data in the East China Sea

The impact of combined assimilation of altimeters data and wave spectra from S-1A and 1B in the operational model MFWAM

Recent improvements on the wave forecasting system of Meteo-France: modeling and assimilation aspects

FORA-WNP30. FORA_WNP30_JAMSTEC_MRI DIAS en

Eddy Shedding from the Kuroshio Bend at Luzon Strait

Coastal Inundation Forecasting and Community Response in Bangladesh

4DVAR Data Assimilation with Chesapeake Bay Operational Forecasting System

Atmospheric circulation analysis for seasonal forecasting

Sea Level Variability in the Western North Pacific during the 20th Century

Comparison of of Assimilation Schemes for HYCOM

AN INTEGRATED MODELING APPROACH FOR SIMULATING OIL SPILL AT THE STRAIT OF BOHAI SEA. Jinhua Wang 1 and Jinshan Zhang 1

HYCOM Caspian Sea Modeling. Part I: An Overview of the Model and Coastal Upwelling. Naval Research Laboratory, Stennis Space Center, USA

Model and observation bias correction in altimeter ocean data assimilation in FOAM

Inter comparison of wave height observations from buoy and altimeter with numerical prediction

Indian Ocean Forecast System (INDOFOS) Abhisek Chatterjee

Recent Data Assimilation Activities at Environment Canada

Sensitivity of Satellite Altimetry Data Assimilation on a Naval Anti-Submarine Warfare Weapon System

An Update on the 1/12 Global HYCOM Effort

Zorana Jelenak Paul S. Chang Khalil Ahmed (OPC) Seubson Soisuvarn Qi Zhu NOAA/NESDIS/STAR-UCAR

Ocean Observations for an End-to-End Seasonal Forecasting System

FORA-WNP30. FORA_WNP30_JAMSTEC_MRI DIAS en

Global climate predictions: forecast drift and bias adjustment issues

Data assimilation for ocean climate studies

PS4a: Real-time modelling platforms during SOP/EOP

Scarborough Tide Gauge

M. Liste 1, M. Grifoll 2, I. Keupers 1, J. Fernández 3, H. Ortega 1, J. Monbaliu 1

SOUTH AFRICAN TIDE TABLES

What is the difference between Weather and Climate?

Surface Anomalies Prior to Earthquakes

Regional eddy-permitting state estimation of the circulation in the Northern Philippine Sea

OPERATIONAL OCEAN FORECAST FOR THE NORTHERN IBERIA PENINSULA (OOF-NIP)

Satellite-derived environmental drivers for top predator hotspots

The Mediterranean Operational Oceanography Network (MOON): Products and Services

Responding to the 2016 and 2017 Mass Coral Bleaching events on the Great Barrier Reef: from Observations to Modelling

Interannual Variability of Wind Induced Onshore Transport over the Northern West Florida Shelf

SST (NRL/NLOM, 28 Sept. 2004) (A global, surface layer product)

IAP Dynamical Seasonal Prediction System and its applications

GRADE 6 GEOGRAPHY TERM 1 LATITUDE AND LONGITUDE (degrees)

Global Ocean Monitoring: Recent Evolution, Current Status, and Predictions

Transcription:

Development and Application of the Chinese Operational Hydrological Forecasting System Guimei LIU National Marine Environmental Forecasting Center, Beijing www.nmefc.gov.cn

Contents Background Operational Ocean Forecasting Systems Data Assimilation Scheme Ocean Services Summary 01 02 03 04 05

Chinese Operational Hydrological Forecasting System 1. Northwest Pacific 2. South China Sea 3. East China Sea 4. Bohai Sea 1 OGCM Horizontal Res. ROMS 1/20 o 1/30 o 1/30 o 1/60 o 4 2 Vertical Res. 30 levels 36 levels 30 levels 30 levels Atmosphere Forcing Assimilation Scheme 3D- VAR GFS/CGOGS-wind/NMEFC-WRF Nudging/EnOI Nudging SST MGDSST 3 OB S SSH Other s Jason-1 & Jason-2, Cryosat, SARAL and HY2 In-situ temperature and salinity profiles, e.g. Argos, XBTs Products Forecast Range Update Frequency Temperature, Salinity, Currents 5 days Daily

02 Operational Ocean Forecasting Systems

2.1 North-west Pacific Model Configuration Region Resolution Time Steps Boundary Condition 8 o S~52 o N;99 o E~160 o E 1/20 o 1/20 o 30 σ-levels Internal 180s;External 6s MOM4 global ocean forecasting system Hindcast Forcing Clim Data Topo Data GFSR 4 daily data SODA climatology data GEBCO(0.5' 0.5'), with observation data corrected in East China Sea

Model Validation Sea Water Level at (120 W, 20 N) from 1992 to 2011 Modeling Obs U v

Products of NwPM Temperature / Salinity / Current

2.2 East China Sea Model Configuration Based on ROMS, Research Area: 114 ~133 E,22 ~41 N Model Domain: the BoHai, YS and the ECS Resolution: 1/30 1/30 (3.5km) 30 sigma levels Bathymetric data: GEBCO & China Coastal data Boundary Data: SODA & NWP 10 tidal constituents (TPXO7) Forcing data: WRF(NMEFC)& GFS River Discharge: Yangtze River

Model Validation Temperature from Section Data NFRDI observation MODEL OBS ECS r=0.89 U-component V-component

Products of ECSM Temperature / Salinity / Current

2.3 South China Sea Model Configuration Region -5 o N 26 o N 98 o E 140 o E Horizontal Resolution 1/30 Vertical Resolution Max Depth 6000 m Min Depth 10 m 36 Layers Topo ETOPO1

Model Validation Comparison with Obs. Aug. 9 ~ Sep. 8 10N 113E 18N Observation Mercator SCSOFS 6N Temp Salt

Products of SCSM Temperature / Salinity / Current

2.4 Bohai Sea Model Region 37 o S~41 o N;117.5 o E~112.5 o E Resolution 1/60 o 1/60 o 30 σ-levels Time Steps Internal 60s;External 2s Clim Data SODA climatology data Topo Data Observation Topography Data Boundary ECS climatology data

Products of BHSM Temperature / Salinity / Current

2.5 Daya Bay Coastal Model Region: 112.3 ~116.7 E 20.4 ~23.0 N Resolution: < 200m Boundary: M 2 S 2 K 1 O 1 N 2 K 2 P 1 Q 1 Unstructured grid of the model

Model Validation M2 S2 K1 O1 Amp Pha Amp Pha Amp Pha Amp Pha Mod. 0.363 255.76 0.155 284.54 0.355 306.55 0.283 250.56 Obs. 0.351 256.56 0.139 287.50 0.338 306.78 0.275 248.74 Bias 0.012-0.8 0.016-3.0 0.017-0.24 0.008 1.82 AE: 0.18 RE: 0.52 Bias: 0.05 SD: 0.19 Temporal evolution of sea level at Huizhou station. Blue line is observations, red line is simulations.

Model calibration Location of observation stations 实测 模拟 相对误差 流速 流向 流速 流向 流速 流向 33.6 114.4 32.8 101.9 3% 13 31.4 126.8 38.0 116.0 17% 10 55.4 111 74.8 89 22% 22 52.4 111.9 74.1 95 17% 17 45.8 128 61.4 107 25% 21 49.9 98.1 58.1 78 20% 20 41.1 86.8 47.4 77 9% 9 32.5 71 37.9 77 6% 6 32.2 60 31.5 77 17% 17 34 55 35.5 77 23% 22 34.1 63 39.8 76 14% 14 37.1 68 42.8 75 7% 7 42.3 74 42.6 72 2% 2 42.5 82 40.6 68 14% 14 40 99 34.9 75 28% 23 40 88 24.5 63 25% 25

Forecast Validation S ~0.5psu T <1.0

03 Data Assimilation Scheme

Data Assimilation Scheme NwPM SLA Ensemble Optimal Interpolation ECSM SST Three Dimensional Variation SCSM Argo

RMSE( C) latitude EnOI Scheme Assimilation Method: EnOI Period: 2011/01/01~2011/12/31 Observation data for assimilation: OSTIA analysis SST product Assimilation cycle: 5 day (at 00:00) Parameter value: alpha=0.3,localization radius: R=150km 41 o N 40 o N 39 o N 38 o N 37 o N 36 o N 35 o N 34 o N 2 1.5 1 22103 22107 22109 22105 22101 22104 22110 22111 22102 22108 22106 118 o E 120 o E 122 o E 124 o E 126 o E longitude RMS error of Model SST against buoy temperature( C) RMSE of Model SST filed against OSTIA SST filed at 2011 Frer run EnOI Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Time(Month) RMS error of Model SST filed against OSTIA SST filed Buoy Free run EnOI improved (%) 22101 1.29 1.01 21.9 22102 0.81 0.90 11.0 22103 2.31 2.07 10.0 22104 1.54 1.41 8.2 22105 1.21 1.09 10.3 22106 1.06 0.94 10.9 22107 1.92 1.36 29.0 22108 1.54 1.24 19.3 22109 1.38 0.90 34.5 22110 1.29 0.96 25.3 22111 1.12 1.14 1.6 average 1.41 1.18 16.5

EnOI Scheme Schematic diagram of running ensemble-sampling at assimilation time t

3DVAR Scheme Data Assimilation of SST Method: 3D-Var Period: 2015/01/01 ~ now Observation data for assimilation: MGDSST (Merged satellite and in situ data Global Daily Sea Surface Temperatures, 1/4 1/4 ) Assimilation cycle: Daily (at 12:00 UTC) 1 st 2 nd 3 rd 4 th 5 th The Errors between simulations and observations Day ME AE RMSE 1 st 0.09 0.51 0.76 2 nd 0.13 0.56 0.79 3 rd -0.04 0.56 0.82 4 th -0.10 0.60 0.87 5 th -0.15 0.62 0.92

3DVAR Scheme Data Assimilation of Argo profiles Method: 3D-Var Period: TEST: 2006/01/01~2006/12/31; Operational Run: 2015/01/01~now. Observation data for assimilation: T/S Argos Profiles Assimilation cycle: Daily (at 00:00 UTC) Temperature at surface The 136 o E section: Temperature Salinity at 150m The 136 o E section: Salinity For temperature, the RMSE decreases from 0.988 C in the SF run to 0.620 C in the AF run, i.e. a 37.21% reduction occurs. For salinity, the RMSE decreases from 0.098 in the SF run to 0.071 in the AF run, i.e. a 27.98% reductions.

04 Ocean Services

Ocean Services Search and Rescue chemicals spill analysis Oil Spill Carbon Cycle OOFS Escort Mission Coastal Tourist Destinations Forecasts Submersible Jiaolong Exploration South China Sea Model

Search and Rescue Forecasts for trajectory of vessels lost motion and drowning person Missing Malaysian flight MH370 emergency forecasting (On March 8, 2014) Emergency forecasting of search and rescue in Xisha islands sea area (On September 29, 2013, "Butterfly Typh" )

Marine hazardous materials transport 8 12 Tianjin Port hazardous materials transport analysis 1. To simulate the surface current Irregular semi-diurnal tides in Bohai bay; Westward at high tide and eastward at low tide in Tianjin Port coastal area. 2. Supposing the chemicals spilled from Sewage outlet to the sea, To forecast the marine area of influence in 72hours. The concentration diffusion process was simulated on high resolution current. Daily mean Bohai Bay Bohai Bay High tide UTC+8 Low tide UTC+8 Tianjin Port explosion Tianjin Port explosion

Carbon Cycle pco2 ---- ecological model and forecast experiment

Environmental Forecasts Forecasts for Travel Channel (20130521) City Wave Temperature City Wave Temperatur e Da Lian Slight 10.7 Maldives Moderate 29.0 Vladivostok Slight 5.9 Cape Town Moderate 16.2 Jeju 17.7 Rio de Moderate 24.2 Slight Janeiro Tokyo Slight 18.4 Lisbon Moderate 17.9 Shanghai Slight 19.1 Barcelona Slight 16.6 Keelung Slight 24.9 Bergen Rough 8.3 San Ya Slight 28.8 Hamburger Very Rough 11.2 Hong Kong Slight 25.8 San Rough 11.6 Francisco Bangkok Slight 31.0 New York Slight 13.0 Singapore Slight 30.9 Sydney Slight 22.4 Dubai Slight 27.7 Hawaii Moderate 25.8 Submersible Jiaolong Exploration Escort Mission in the Strait of Malacca

Hong Kong-Zhuhai-Macau/Macao Bridge 0 0.2 0.4 0.6 0.8 1 1.2 1.4 1.6 18:00 19:00 20:00 21:00 22:00 23:00 0:00 1:00 2:00 3:00 4:00 5:00 6:00 7:00 8:00 9:00 10:00 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 20:00 21:00 22:00 23:00 0:00 1:00 2:00 3:00 4:00 5:00 6:00 7:00 8:00 9:00 10:00 11:00 12:00 13:00 14:00 15:00 16:00 17:00 18:00 19:00 20:00 21:00 22:00 23:00 0:00 1:00 2:00 3:00 4:00 5:00 6:00 7:00 8:00 9:00 10:00 11:00 12:00 13:00 14:00 15:00 16:00 17:00 4# model

05 Summary

Summary The Operational Ocean Forecasting System of China Sea, which include Northwest Pacific Model, East China Sea Model and South China Sea Model, has been used for operational forecasting everyday. 01 02 The release of Operational Ocean Forecasting System have been applied well to ecological, oil spill forecasting, search and rescue, such as chlorophyll-a, nutrients in the north Pacific, CO 2 flux in the northwest Pacific Ocean, oil explosion in coastal areas, searching for MH370, and so on. 03 In the further work, extension of forecast range, development of forecast system with independent intellectual property, construction of observation system will be considered more and more.

www.nmefc.gov.cn