NOAA ESRL PSD Briefing March 2013 Surface Processes and Coupled Modeling Light Winds to Hurricanes Poles to Tropics Momentum, Heat, Moisture, Trace Gases,

Slides:



Advertisements
Similar presentations
Basics of numerical oceanic and coupled modelling Antonio Navarra Istituto Nazionale di Geofisica e Vulcanologia Italy Simon Mason Scripps Institution.
Advertisements

NOAA in the Antarctic James H. Butler, Director Global Monitoring Division Earth System Research Laboratory National Oceanic and Atmospheric Administration.
NOAA COARE Gas Transfer parameterization: Update Using Wave Parameters C. W. Fairall* NOAA Earth Science Research Laboratory, Boulder, CO, USA Ludovic.
Climate modeling Current state of climate knowledge – What does the historical data (temperature, CO 2, etc) tell us – What are trends in the current observational.
UNIVERSITY OF LEEDS School of Earth and Environment INSTITUTE FOR CLIMATE AND ATMOSPHERIC SCIENCE Arctic Summer Cloud-Ocean Study (ASCOS) Ian Brooks, Cathryn.
METR112-Climate Modeling
THORPEX-Pacific Workshop Kauai, Hawaii Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio David H. Bromwich.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
METR112-Climate Modeling Basic concepts of climate Modeling Components and parameterization in the model sensitivity of the model.
Global Warming. what is global warming ? Global warming is the increase in average temperature of the oceans and air near the earth's surface occurred.
Evaporative heat flux (Q e ) 51% of the heat input into the ocean is used for evaporation. Evaporation starts when the air over the ocean is unsaturated.
Overview II: Importance of the atmospheric boundary layer.
Arctic System Model WorkshopBoulder, Colorado Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio David H. Bromwich.
CALWATER2 Field Study of Air-Sea Interaction and AR dynamics in Midlatitude Pacific Storms Ship (NOAA Brown) Ship Field Duration – 30 days Time Window.
National Center for Atmospheric Research * ASP Summer Colloquium * Boulder Colorado * June 1, 2009 University of Colorado at Boulder Boundary Layer Lecture.
Mesoscale Modeling Review the tutorial at: –In class.
Ship-based measurements of cloud microphysics and PBL properties in precipitating trade cumulus clouds during RICO Allen White and Jeff Hare, University.
Atmospheric Modeling in an Arctic System Model John J. Cassano Cooperative Institute for Research in Environmental Sciences and Department of Atmospheric.
WWRP Polar Prediction Project Thomas Jung Chair of the WWRP Polar Prediction Project Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research.
Surface and Boundary-Layer Fluxes during the DYNAMO Field Program C. Fairall, S. DeSzoeke, J. Edson, + Surface cloud radiative forcing (CF) Diurnal cycles.
Presentation Slides for Chapter 1 of Fundamentals of Atmospheric Modeling 2 nd Edition Mark Z. Jacobson Department of Civil & Environmental Engineering.
Questions for Today:  What is Weather and Climate?  What are four major factors that determine Global Air Circulation?  How do Ocean Currents affect.
Automated Weather Observations from Ships and Buoys: A Future Resource for Climatologists Shawn R. Smith Center for Ocean-Atmospheric Prediction Studies.
MOSAiC Multidisciplinary drifting Observatory for the Study of Arctic Climate Matthew Shupe – U. of Colorado Ola Persson – U. of Colorado Michael Tjernström.
Jian-Wen Bao Christopher W. Fairall Sara A. Michelson Laura Bianco NOAA/ESRL/Physical Sciences Division in collaboration with N. Surgi, Y. Kwon and V.
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Science Discipline Overview: Atmosphere (large-scale perspective)  How might large-scale atmospheric challenges add to the scientific arguments for MOSAIC?
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.
© Crown copyright Met Office The Role of Research Aircraft in YOPP Chawn Harlow, YOPP Summit, WMO, Geneva 13 July 2015.
R. A. Brown 2003 U. Concepci Ó n. High Winds Study - Motivation UW PBL Model says U 10 > 35 m/s Composite Storms show high winds Buoy limits:
Climate: It’s All About the Sun!!! Or, Is It? Chris Fairall, NOAA ESRL Introduction, background on climate system Black body radiation basics The sun vs.
Air – Sea Measurements from Ships: Fluxes, Time Series, Remote Sensing Dr. Jeff Hare CIRES – University of Colorado and NOAA Earth Systems Research Lab.
Overview of NOAA’s Arctic Climate Science Activities Current or Proposed Activities Expected to Persist in FY
Bulk Parameterizations for Wind Stress and Heat Fluxes (Chou 1993; Chou et al. 2003) Outlines: Eddy correlation (covariance) method Eddy correlation (covariance)
Working Group on Surface Fluxes In situ issues Elizabeth Kent National Oceanography Centre, Southampton.
There was a notable difference in atmospheric ozone concentrations during the cruises. The lowest ozone mixing ratios were measured in the Southern Atlantic.
Arctic Research Office May, 2002 Update on SEARCH from the Agency Perspective.
Robert Wood, Atmospheric Sciences, University of Washington The importance of precipitation in marine boundary layer cloud.
Evaluation of the Accuracy of in situ Sources of Surface Flux Observations for Model Validation: Buoys and Research Vessels in the Eastern Pacific C. W.
Physics of Sea Spray Scott W. Powell 1,2, Jian-Wen Bao 1, Christopher W. Fairall 1, Laura Bianco 1 1 NOAA/ESRL/PSD, Boulder, Colorado 2 Rosenstiel School.
Ocean Surface heat fluxes
Modeling and Evaluation of Antarctic Boundary Layer
Effect of the Gulf Stream on Winter Extratropical Cyclones Jill Nelson* and Ruoying He Marine, Earth, and Atmospheric Sciences, North Carolina State University,
Multidisciplinary drifting Observatory for the Study of Arctic Climate
Parameterizations of the Sea-Spray Effects
The Multidisciplinary drifting Observatory
RIME A possible experiment for Advancing Antarctic Weather Prediction David H. Bromwich 1, John J. Cassano 1, Thomas R. Parish 2, Keith M. Hines 1 1 -
CLAWATER2 Ship-based Field Study of Air-Sea Interaction in Midlatitude Pacific Storms One ships (Brown? Or UNOLS Class I) Aircraft (NOAA P-3, NASA Global.
© Crown copyright Met Office WGNE activities and future directions Andy Brown.
Measurement and Parameterization of Air-Sea Gas Transfer over the Southern Ocean in GasEx-III C. W. Fairall, J. E. Hare, Ludovic Bariteau, ESRL- CIRES/Univ.
Atm S 547 Lecture 1, Slide 1 The Atmospheric Boundary Layer (ABL or PBL) The layer of fluid directly above the Earth’s surface in which significant fluxes.
Observations of Air-sea Interaction in the Northeast Tropical Atlantic C.W. Fairall, L. Bariteau, S. Pezoa, D. Wolfe NOAA/ Earth System Research Laboratory,
NAME SWG th Annual NOAA Climate Diagnostics and Prediction Workshop State College, Pennsylvania Oct. 28, 2005.
Importance of the atmospheric boundary layer (2).
How Convection Currents Affect Weather and Climate.
MOSAiC Meeting, ASSW, 13 March 2016, Fairbanks Townhall Meeting 13 March :00 – 17:00 Multidisciplinary drifting Observatory for the Study of Arctic.
Precipitation Effects on Turbulence and Salinity Dilution in the Near Surface Ocean Christopher J. Zappa Lamont-Doherty Earth Observatory, Columbia University,
ESSL Holland, CCSM Workshop 0606 Predicting the Earth System Across Scales: Both Ways Summary:Rationale Approach and Current Focus Improved Simulation.
A New Climatology of Surface Energy Budget for the Detection and Modeling of Water and Energy Cycle Change across Sub-seasonal to Decadal Timescales Jingfeng.
The Atmosphere Today, human activity is altering the quantities of some of these variable gases CO2 CH4 N2O O3 CFCs.
Tropical Convection and MJO
Climate.
The Atmosphere during MOSAiC
Air-Sea Interaction: Physics of air-surface interactions and coupling to ocean/atmosphere BL processes Emphasize surface fluxes Statement of problem Present.
Atmosphere & Weather Review
Shuyi S. Chen, Ben Barr, Milan Curcic and Brandon Kerns
Mark A. Bourassa and Qi Shi
Annual cycle of cloud fraction and surface radiative cloud forcing in the South-East Pacific Stratocumulus region Virendra P. Ghate and Bruce A. Albrecht.
Roberto Mechoso and I. Richter
Presentation transcript:

NOAA ESRL PSD Briefing March 2013 Surface Processes and Coupled Modeling Light Winds to Hurricanes Poles to Tropics Momentum, Heat, Moisture, Trace Gases, Aerosol Particles, Radiation, Precipitation Christopher W. Fairall 1, Jim Wilczak 1, Jian-Wen Bao 1, Andrey A. Grachev 1, 2, Jeff Hare 1, 2, Ludovic Bariteau 1, 2, Ola Persson 1, 2 1 NOAA Earth System Research Laboratory/Physical Science Division, Boulder, Colorado, USA 2 Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado1

Building Blocks Direct measurements Surface flux parameterizations Boundary Layers Turbulent transport Microphysics Coupled models Hurricane Sea-ice MJO April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado2

BACKSTORY 1996 Release COARE2.5 bulk flux algorithm 2002 Chris Bretherton evaluating coupled climate model asks ‘Which one of these flux maps is right?” 2003 WCRP Working Group on Surface Fluxes (CWF chair) 2005 WHOI global flux product 2011 COAREG3.1 CO2, DMS, 3 He, CO, O 3, SF 6 and 73 other gases 2013 GOV/WGNE Coupled Prediction Workshop, NCEP:’So where can we get these flux data?’ April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado3

APPROACH Direct data used principally to develop parameterizations, improve the observing system, and ‘verify’ model results Direct Flux Observations Tech Development, Near- surface, Boundary-Layer Observations Fundamental Physics Navier-Stokes, Turbulent Kinetic Energy budget equations, scalar conservation Flux Parameterization Similarity scaling, cloud-radiative coupling, deposition velocities Research Numerical Models 1-D Closure, Large Eddy Simulation, Mesoscale, Cloud Resolving, Regional Ocean Flux Observing System Research Vessels (SAMOS), Ship Opportunity (COADS), Flux Reference Buoys (OceanSites), Satellites (SEAFLUX ) NOAA Models Operational Numerical Weather Prediction Climate Models April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado4

TECHNOLOGY EXAMPLE: Motion-Corrected Eddy- Covariance Turbulence Measurements from Ships April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado5

Surface Turbulent Flux Parameterizations Turbulent Fluxes: Bulk Parameterization Flux= Mean correlation of turbulent variables, MetFlux – Dominated by atmospheric turbulent transfer physics GasFlux – Dominated by oceanic molecular transfer physics; Enhanced by whitecap bubbles Transfer coefficients computed from direct flux measurements April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado6

NOAA COARE AIR SEA TURBULENT FLUX MODEL 1996 Bulk Meteorological fluxes Update 2003 (7200 covariance obs*) Oceanic cool skin Ocean diurnal warm layer 2000 CO 2 [U. Conn and Columbia U] 2003 Hurricane Sea Spray 2004 DMS [U. Hawaii] 2005 Snow/Ice [US Army CRREL] 2006 Ozone [U. Colorado] 2008 PCBs and PCEs [Mich. Tech. U] 2009 Hurricanes [UNSW Australia] Trace gases 2011 COAREG3.1 CO2, DMS, 3 He, CO, O 3, SF 6 PSD cruises Pacific Ocean *Complete flux data time series publically available under ‘Data Sets’ at April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado7 Close to 2000 literature citations

Drag Coefficient at High Wind Speed April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado8

Programatic View CPO SEARCH Arctic Observatories (T.Uttal) k$1000 Ocean ObsFlux observing system 300 Air-SeaEPIC, NAME, VOCAL,DYNAMO150 Gas fluxGasex I, II, III, ?? (100) Hurricanes NOAA BasePhysics, P-3observations 650 HFIPHWRF physics (Bao) 100 NASAGOES-5 fluxes 100 NOPPModel flux coupler0 Renewable energyDOE WFIP (Wilczak)/GSD RUC 300 Arctic Persson, Shupe, Solomon, Grachev NSF, DOE BL, mesoscale, microphys, WRF 600 ONRWaves-ice interactions 200 April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado9

Surface Processes and Coupled Models: Wider Contex 2009 OceanOBS09 WP Flux Observing Sys 2011 WMO Polar Pred. Steering Committee 2012 MOSAIC plans 2-yr Arctic Obs Station 2012 US-IOOS12 WP CoastalFlux Observing 2012 GSOP/CLIVAR Ocean reanalysis and fluxes 2013 WGNE/GOV WP on Obs for Coupled Predictions 2013 BAMS High latitude fluxes April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado10

The Future Arctic WWRP Polar Predictions (International effort) 7 major field programs BOEM/PSD-GSD (Intrieri) initiative sea ice predictions SEARCH TIKSI observatory completion (??) NOAA P-3 surface interaction Observations Wband radar, WSRA wave measurements, Video… Surface fluxes, sea spray, WaveWatch-III Air-Sea/CPO CALWATER2 – follow on to DYNAMO Flux products for coupled models Renewable energy Four more WFIP’s? (complex, ocean, coastal, island) April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado11

ISSUES Arctic is major upswing SEARCH cut k$420 in FY13 because???. FY14? Support for PPP? ESRL participation non-NOAA funds? Havent been able to get the R/V Ron Brown since Took observing systems off. Transferred C-band radar to CSU. ‘Penciled in’ for CALWATER2 2015, but remain skeptical Worry about follow thru on DYNAMO. Need another round of grants. Loss of base-funded hours on P-3 gets worse every year. Got P-3 for DYNAMO because ONR paid 1m$ Renewable energy – will NOAA drop the ball? April 1, 2013 PageNOAA Earth System Research Laboratory- Boulder, Colorado12