Atmospheric data for Arctic modeling John Walsh International Arctic Research Center University of Alaska, Fairbanks Arctic System Modeling Workshop, Montreal,

Slides:



Advertisements
Similar presentations
Development of Bias-Corrected Precipitation Database and Climatology for the Arctic Regions Daqing Yang, Principal Investigator Douglas L. Kane, Co-Investigator.
Advertisements

What is a Synoptic Weather Map?
w4fg&feature=related.
Weather Station Models What do they mean? How do you translate them?
S4D WorkshopParis, France Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio A High-Resolution David H. Bromwich.
NATS 101 Lecture 3 Climate and Weather. Climate and Weather “Climate is what you expect. Weather is what you get.” -Robert A. Heinlein.
THORPEX-Pacific Workshop Kauai, Hawaii Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio David H. Bromwich.
Weather Forecasting – The Traditional Approach Pine cones open and close according to air humidity. An open pine cone means dry weather. Ash leaf before.
A few last-minute things…. Rossby wave breaking...
Atmospheric Sciences 370 Observing Systems January 2007.
1 NATS 101 Lecture 3 Climate and Weather. 2 Review and Missed Items Pressure and Height-Exponential Relationship Temperature Profiles and Atmospheric.
Foundation Sea Surface Temperature W. Emery, S. Castro and N. Hoffman From Wikipedia: Sea surface temperature (SST) is the water temperature close to the.
 Global Integrated Polar Prediction System (GIPPS)  The WWRP Polar Prediction Project (PPP)  The WCRP Polar Climate Predictability Initiative (PCPI)
Adrian Simmons Lead author, Status Report for the Global Climate Observing System Consultant, European Centre for Medium-Range Weather Forecasts Surface.
Matthew Shupe Von Walden David Turner U. Colorado/NOAA-ESRL U. Idaho NOAA - NSSL New Cloud Observations at Summit, Greenland: Expanding the IASOA Network.
Dr Mark Cresswell Model Assimilation 69EG6517 – Impacts & Models of Climate Change.
Arctic System Model WorkshopBoulder, Colorado Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio David H. Bromwich.
General comments Need for new observations versus new parameterizations? Should explore what GCOS and others are doing Urgent need for concerted physical.
© The Aerospace Corporation 2014 Observation Impact on Mesoscale Model Forecast Accuracy over Southwest Asia Dr. Michael D. McAtee Environmental Satellite.
Utilization of Observations at the Russian Drifting Stations “North Pole” for Improved Description of Air–Sea-Ice-Ocean Interactions in the Arctic Ocean.
MADIS to LITTLE_R Converter MADIS observation types MADIS to LITTE_R converter Future work.
1 Aircraft Data: Geographic Distribution, Acquisition, Quality Control, and Availability Work at NOAA/ESRL/GSD and elsewhere.
The Tiksi Hydrometeorological Observatory Program International Collaboration for Climate Studies U.S. Science Contact:
Collaborative Research: Toward reanalysis of the Arctic Climate System—sea ice and ocean reconstruction with data assimilation Synthesis of Arctic System.
Automated Weather Observations from Ships and Buoys: A Future Resource for Climatologists Shawn R. Smith Center for Ocean-Atmospheric Prediction Studies.
1 NOAA and the International Polar Year A Presentation to the NOAA Science Advisory Board Dr. John A. Calder Director Arctic Research Office March 23,
Why We Care or Why We Go to Sea.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
Synthesis NOAA Webinar Chris Fairall Yuqing Wang Simon de Szoeke X.P. Xie "Evaluation and Improvement of Climate GCM Air-Sea Interaction Physics: An EPIC/VOCALS.
1 AISC Workshop May 16-18, 2006 Lesson Learned from CCSP 1.1: Temperature Trends in the Atmosphere Lesson Learned from CCSP 1.1 Temperature Trends in the.
Arctic System Reanalysis David H. Bromwich 1,2 and Keith M. Hines 1 1- Polar Meteorology Group Byrd Polar Research Center The Ohio State University Columbus,
RICO Modeling Studies Group interests RICO data in support of studies.
Overview of NOAA’s Arctic Climate Science Activities Current or Proposed Activities Expected to Persist in FY
Current and Future Use of Satellite Data in NWP at Environment Canada Satellite Direct Readout Conference 2011 Miami, USA David Bradley, Gilles Verner,
Current and Future Initialization of WRF Land States at NCEP Ken Mitchell NCEP/EMC WRF Land Working Group Workshop 18 June 2003.
Weather 101 Brainstorm Why do we study the weather? Create a concept map with as many words you know about weather.
Autonomous Polar Atmospheric Observations John J. Cassano University of Colorado.
1 Developing Assimilation Techniques For Atmospheric Motion Vectors Derived via a New Nested Tracking Algorithm Derived for the GOES-R Advanced Baseline.
EGY Meeting, Boulder, Colorado March 13-14, 2007 FRESH PERSPECTIVES Ron Weaver NSIDC, University of Colorado, Boulder.
Evaluation of the Real-Time Ocean Forecast System in Florida Atlantic Coastal Waters June 3 to 8, 2007 Matthew D. Grossi Department of Marine & Environmental.
Point Comparison in the Arctic (Barrow N, 156.6W ) Part I - Assessing Satellite (and surface) Capabilities for Determining Cloud Fraction, Cloud.
Retrieval Algorithms The derivations for each satellite consist of two steps: 1) cloud detection using a Bayesian Probabilistic Cloud Mask; and 2) application.
NCEP Data Reanalysis 陳漢卿. Data analyses Use the data available for the original operational NCEP analyses. (available from 1962) Add other datasets to.
NCAR April 1 st 2003 Mesoscale and Microscale Meteorology Data Assimilation in AMPS Dale Barker S. Rizvi, and M. Duda MMM Division, NCAR
Module 17 MM5: Climate Simulation BREAK. Regional Climate Simulation for the Pan-Arctic using MM5 William J. Gutowski, Jr., Helin Wei, Charles Vörösmarty,
Station Models and Converting Station Pressure into Millibars.
MODIS Winds Assimilation Impact Study with the CMC Operational Forecast System Réal Sarrazin Data Assimilation and Quality Control Canadian Meteorological.
Atmospheric Sciences 370 Observing Systems January 2012.
Inversions. Usually temperature decreases with height by approximately 5.5 C per km But with high pressure, clear or near clear skies, and light winds,
Instruments. In Situ In situ instruments measure what is occurring in their immediate proximity. E.g., a thermometer or a wind vane. Remote sensing uses.
EuroGOOS Arctic Task Team Workshop September 2006 Satellite data portals for Arctic monitoring Stein Sandven Nansen Environmental and Remote Sensing.
Status Report: NOAA’s Arctic Goals for IPY & Beyond John Calder and Kathleen Crane Arctic Research Program, CPO Office of Oceanic and Atmospheric Research.
Atmospheric Sciences 370 Observing Systems Winter 2016.
Reducing Canada's vulnerability to climate change - ESS Towards a water budget for Canada: are reanalyses suitable for the task?
Use of high resolution global SST data in operational analysis and assimilation systems at the UK Met Office. Matt Martin, John Stark,
Station lists and bias corrections Jemma Davie, Colin Parrett, Richard Renshaw, Peter Jermey © Crown Copyright 2012 Source: Met Office© Crown copyright.
June 20, 2005Workshop on Chemical data assimilation and data needs Data Assimilation Methods Experience from operational meteorological assimilation John.
IASC Workshop Potsdamr, Germany Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio, USA The Arctic System Reanalysis.
AON enables the U.S. Study of Environmental ARctic CHange (SEARCH) GOALS: record the full suite of changes inform research on the causes and consequences.
Weather Station Model.
International Arctic System for Observing the Atmosphere (IASOA)
A Brief Introduction to CRU, GHCN, NCEP2, CAM3.5
Assimilation of GOES-R Atmospheric Motion Vectors
Group interests RICO data required
Research Data Archives at NCAR
Comparison of Aircraft Observations With Surface Observations from
NATS 101 Lecture 3 Climate and Weather
Group interests RICO data in support of studies
New York State Mesoscale Weather Network
NATS 101 Lecture 3 Climate and Weather
Presentation transcript:

Atmospheric data for Arctic modeling John Walsh International Arctic Research Center University of Alaska, Fairbanks Arctic System Modeling Workshop, Montreal, July 2009

Three categories of atmospheric observations: 1)Routine measurements for input to NWP models 2) Special observing networks 3)Short-duration field campaigns

Three categories of atmospheric observations: 1)Routine measurements for input to NWP models 2) Special observing networks 3)Short-duration field campaigns + Value-added products: reanalyses gridded fields (e.g., CRU) Polar Pathfinder products

Routine measurements – in some respects, the Arctic is well-covered  surface synoptic network  rawinsonde network  buoy, ship reports  aircraft reports  satellite measurements (profiles of T, q, wind)  Archived in reanalysis ingest data banks (e.g., PREPBUFR files at NCAR)

Surface station observationsUpper-air rawinsonde observations

Surface ship and ocean buoy reports 7-days

Reports from commercial, military, and reconnaissance sources 7-days: 01/01/ /07/2003

Satellite-derived temperatures 7-days Winds derived from satellite observed cloud drift analysis 7-days

6-hour accumulated observations: red: surface station slate blue: upper-air yellow: sat. temp. green: sat. wind violet: aircraft sky blue: ship 01/01/ Z

6-hour accumulated observations: red: surface station slate blue: upper-air yellow: sat. temp. green: sat. wind violet: aircraft sky blue: ship 01/01/ Z

6-hour accumulated observations: red: surface station slate blue: upper-air yellow: sat. temp. green: sat. wind violet: aircraft sky blue: ship 01/01/ Z

6-hour accumulated observations: red: surface station slate blue: upper-air yellow: sat. temp. green: sat. wind violet: aircraft sky blue: ship 01/01/ Z

SID=BAW269, YOB= 60.00, XOB=340.00, ELV=10058, DHR=-0.550, RPT= , TCOR=0, TYP=130, TSB=0, T29= 41, ITP=99, SQN= 26 PROCN= 0, SAID=*** RCT= 18.08, PCAT=*****, POAF=***, DGOT=*** level 1 obs qmark qc_step rcode fcst anal oberr category PRESSURE (MB) PREPRO ***** ******** ******** ******** 6. SP HUMIDITY(MG/KG) ******** ****** ***** ******** 6. TEMPERATURE (C) PREPACQC TEMPERATURE (C) PREPRO ***** HEIGHT (METERS) PREPRO ***** ******** 6. U-COMP WIND (M/S) PREPACQC U-COMP WIND (M/S) PREPRO ***** V-COMP WIND (M/S) PREPACQC V-COMP WIND (M/S) PREPRO ***** WIND DIR (DEG) ****** PREPRO ***** ******** ******** ******** 6. WIND SPEED (KNOTS) 10.0 ****** PREPRO ***** ******** ******** ******** 6. Sample PrepBUFR observations: SID=48582, YOB= 82.85, XOB=194.99, ELV= 0, DHR= 1.883, RPT= , TCOR=0, TYP=180, TSB=*, T29=562, ITP=99, SQN= 203 PROCN= 2, SAID=*** PMO=******, PMQ=** level 1 obs qmark qc_step rcode fcst anal oberr category PRESSURE (MB) PREPRO ***** SP HUMIDITY(MG/KG) ******** ****** ***** ******** 0. TEMPERATURE (C) PREPRO ***** HEIGHT (METERS) PREPRO ***** ******** 0.

PrepBUFR data Quality Control Flags 0) Keep (always assimilate) 1)Good 2)Neutral or not checked (default) -- e.g., IAOBP T and P obs are flagged as QC=2 3)Suspect 4)Rejected (don’t assimilate) ** Rejected obs. have an additional flag layer indicating justification (e.g., conflicts with a pre-existing QC=0; threshold test failure, etc.)

2) Examples of special observing networks International Arctic Buoy Network ( + Russian NP stations) Greenland automated weather stations Trace gas/chemical sampling (NOAA CMDL) Baseline Surface Radiation Network (BSRN), ARM International Arctic System for Observing the Atmosphere (IASAO)

Tiksi, Russia Alert, CanadaBarrow, Alaska Eureka, Canada Summit, Greenland Ny-Alesund, Svalbard IASOA Target Observatories IASAO

IASAO: International Arctic System for Observing the Atmosphere

3) Short-duration field programs -- process studies for algorithm development, model validation SHEBA ATLAS, LAII Flux Study ARM field campaigns OASIS IPY cruises … others

Problem areas Precipitation, especially solid precip (snowfall, depth, water equivalent) Clouds Aerosols … others