Antarctic Regional Interactions Meteorology Experiment (RIME) Antarctic Regional Interactions Meteorology Experiment (RIME) David H. Bromwich 1, John J.

Slides:



Advertisements
Similar presentations
Essentials of Oceanography
Advertisements

S. E. Stammerjohn, M. R. Drinkwater, R. C. Smith, and X. Liu Presented by Brad Goodwin Atmospheric Science Graduate Student.
Climatology and Variability of Mesoscale Cyclones in the Western Antarctic Peninsula Region Dan Lubin Scripps Institution of Oceanography Rob Wittenmyer.
El Niño, La Niña and the Southern Oscillation
Class #7: Thursday, July 15 Global wind systems Chapter 10 1Class #7, Thursday, July 15, 2010.
 Bodies of air that bring distinctive weather features to the country.  A mass of air in air that is very uniform in temperature, pressure, and humidity.
An Analysis of the Low-Level Wind Field Over the Ross Ice Shelf, Antarctica Melissa A. Richards (Nigro) John J. Cassano University of Colorado.
THORPEX-Pacific Workshop Kauai, Hawaii Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio David H. Bromwich.
El Niño/Southern Oscillation Major climatic perturbation on the planet Coupled atmosphere ocean process Key is the western tropical Pacific – Ascending.
Oceans, Currents, and Weather Dynamics
MET 61 1 MET 61 Introduction to Meteorology. MET 61 2 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 11 Global Circulation.
Mesoscale Convective Systems Robert Houze Department of Atmospheric Sciences University of Washington Nebraska Kansas Oklahoma Arkansas.
Validating the moisture predictions of AMPS at McMurdo using ground- based GPS measurements of precipitable water Julien P. Nicolas 1, David H. Bromwich.
Implementation of the Ross Island Meteorology Experiment (RIME) Implementation of the Ross Island Meteorology Experiment (RIME) David H. Bromwich 1, John.
Gyres and Currents Made by Michael Kramer.
Climate and Climate Change. Climate Climate is the average weather conditions in an area over a long period of time. Climate is determined by a variety.
Question and Answer Session Related to the Weather photo: D. Martin Douglas K. Miller Professor and Chair Atmospheric Sciences Department UNC Asheville.
Class #13 Monday, September 27, 2010 Class #13: Monday, September 27 Chapter 7 Global Winds 1.
Making Connections Chapter 12
Satellites, Weather and Climate Module ??: Polar Vortex.
The polar sea ice covers are large Tens of millions of square kilometers, and empty.
ANTCI Overall Objective To provide a more comprehensive understanding of Antarctic atmospheric chemistry with the goal of providing new insights related.
Chapter 7 Circulation of the Atmosphere A Synoptic-scale Event.
Polar Prediction The Scientific Challenges - Antarctica John Turner British Antarctic Survey Cambridge, UK.
Imposed versus Dynamically Modeled Sea Ice: A ROMS study of the effects on polynyas and waters masses in the Ross Sea John M. Klinck, Y. Sinan Hüsrevoglu.
Long-Term Changes in Northern and Southern Annular Modes Part I: Observations Christopher L. Castro AT 750.
The General Circulation of the Atmosphere and Oceans ATS 351 Lecture 9 November 2, 2009.
Progress of US CLIVAR during Reasons for recapping progress: - Present advances in scientific understanding of the climate system - Demonstrate.
Southern Oscillation- Atmospheric component of ocean's El Niño. Oscillation in the distribution of high and low pressure systems across the equatorial.
Regional Modeling of Antarctic Clouds Keith M. Hines 1 and David H. Bromwich 1,2 1 Polar Meteorology Group Byrd Polar Research Center The Ohio State University.
Autonomous Polar Atmospheric Observations John J. Cassano University of Colorado.
International Workshop on Antarctic Clouds Columbus, OH Polar Meteorology Group, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio.
1 Opposite phases of the Antarctic Oscillation and Relationships with Intraseasonal to Interannual Activity in the Tropics during the Austral Summer (submitted.
The General Circulation  The large-scale wind patterns of the earth  Mission: to mitigate global temperature contrasts (decrease temperature gradients,
The Ross Island Meteorology Experiment (RIME): An International Collaborative Investigation of Antarctic Meteorology and Climate David Bromwich Polar Meteorology.
Global Wind Patterns. What is Wind? Wind is the movement of air from an area of higher pressure to an area of lower pressure. Warmer air expands, becoming.
Understanding Air Pressure
The Ross Island Meteorology Experiment (RIME): An International Collaborative Investigation of Antarctic Meteorology and Climate David Bromwich Polar Meteorology.
Ocean Systems and Climate Modification Ocean Systems Summary Ocean Response Issues ©2001, Perry Samson, University of Michigan.
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 -
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
SeaWiFS Views Equatorial Pacific Waves Gene Feldman NASA Goddard Space Flight Center, Lab. For Hydrospheric Processes, This.
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
Real-time forecasting for the Antarctic: An evaluation of the Antarctic Mesoscale Prediction System (AMPS) David H. Bromwich 1, Andrew J. Monaghan 1, Kevin.
Oceans and Climate IB Geography. Distance from the sea and Weather Due to the differing specific heat capacities of land and water, this can affect local.
Class #17 Monday, February 16, Class #17: Monday, February 16 Surface pressure and winds Vertical motions Jet streams aloft.
Climatic Changes. Standards 4d: Students know the differing Greenhouse conditions on Earth, Mars and Venus; the origins of those conditions; and the climatic.
AMPS Update – July 2010 Kevin W. Manning Jordan G. Powers Mesoscale and Microscale Meteorology Division NCAR Earth System Laboratory National Center for.
Wind.
Oceans.
Global Weather Patterns
Climatic Interactions
Oliver Elison Timm ATM 306 Fall 2016
Understanding Air Pressure
Daylength Local Mesoscale Winds Chinook Winds (Foehn) Loma, MT: January 15, 1972, the temperature rose from -54 to 49°F (-48 to 9°C), a 103°F (58°C)
Air-Sea Interactions The atmosphere and ocean form a coupled system, exchanging heat, momentum and water at the interface. Emmanuel, K. A. 1986: An air-sea.
Natural Climate Variability
100 pt 100 pt 100 pt 100 pt 100 pt 200 pt 200 pt 200 pt 200 pt 200 pt
The ACCIMA Project - Coupled Modeling of the High Southern Latitudes
El Niño and La Niña.
University of Colorado – Boulder
EL NINO Figure (a) Average sea surface temperature departures from normal as measured by satellite. During El Niño conditions upwelling is greatly.
Understanding Air Pressure
Chapter 19.3 Regional Wind Systems.
General Atmospheric Circulation
Chapter 10 Wind: Global Systems.
Ocean Currents Some key questions: What causes the ocean currents?
Characteristics of El Niño
Presentation transcript:

Antarctic Regional Interactions Meteorology Experiment (RIME) Antarctic Regional Interactions Meteorology Experiment (RIME) David H. Bromwich 1, John J. Cassano 2, James Pinto 2,3, and James Moore 4 1 -Ohio State University 2 -University of Colorado Boulder 3 -NCAR Atmospheric Technology Division 4 -UCAR Joint Office for Scientific Support Outline Key science questions Approaches to address key science questions Timeline Budget aspects Discussion topics

The Overarching Hypothesis: The Ross Sea region is critical in the transport of mass, heat and momentum between the Antarctic continent and lower latitudes of the Southern Hemisphere on a variety of scales.

Figure 2.1. Mean streamlines of the wind at approximately 10-m above the surface based on daily MM5 simulations from 15 June – 15 July Surface interactions with middle latitudes (Courtesy Thomas R. Parish) Ross Ice Shelf Air Stream (RAS) Siple Coast Circumpolar Vortex Byrd Glacier Terra Nova Bay

Mass loss from Antarctica primarily via the Ross Sea Sector has hemispheric impact Parish and Bromwich (1998) (Zonal average includes all longitudes)

Surface Pressure DifferenceSurface Temperature Difference Tropical teleconnections: Late 1990s El Nino minus La Nina **The Ross Sea is a center of action (Bromwich et al. 2004)

Specific science topics Boundary-Layer Structure and TransformationBoundary-Layer Structure and Transformation Local Moist Atmospheric ProcessesLocal Moist Atmospheric Processes Mesoscale CyclonesMesoscale Cyclones Terrain-Induced CirculationsTerrain-Induced Circulations Moist Processes and Cyclonic EventsMoist Processes and Cyclonic Events Circumpolar VortexCircumpolar Vortex Hemispheric InteractionsHemispheric Interactions Antarctica Ross Ice Shelf South Pacific Ocean Rising motion due to cyclones Katabatic Winds RAS = Katabatic + Barrier Winds Southward Return Flow Sinking Branch Polar Direct Circulation over Antarctica: Emphasizing the Ross Sea How do these topics relate to climate?

Approaches to address science questions Investigation Approaches Regional Surface- Based Array RIME Supersite Aircraft StudiesModeling Satellite Remote Sensing Climate Studies Small scale Boundary Layer Structure and Transformation xxxx Local Moist Atmospheric Processes xxxxx Mesoscale Cyclones xxxxx Terrain- Induced Circulations xxxx x Moist- Processes and Cyclonic Events x xxxx Circumpolar Vortex x xxxx Science Topics Large scale Hemispheric Interactions xxxx

RIME Field Sites: RIME Supersite Planned AWS sites Planned radiosonde sites New AWS sites Existing research stations Ice Shelf Edge South Pole traverse route 500 km

Ross Ice Shelf MG Pattern Meso Raster RAS MG Pattern Local Raster Glacier Pattern Aircraft flight track schematics showing regional and local scale sampling strategies. Long distance/duration C-130 and HIAPER flights to address local and regional process studies. Mapping of local airflow components and RAS accomplished with C-130, Aerosondes and twin otters. (sawtooth, glacier pattern, local raster, meso raster and MG pattern). Aircraft measurements will complement simultaneous Supersite, special AWS and sounding measurements in the region. RIME Aircraft Activities to address key phenomena and scale interactions: Supersite

Timeline: RIME Field Activities and Science Topics Circumpolar Vortex Terrain-Induced Circulations Moist Processes and Cyclonic Events Mesoscale Cyclones Boundary Layer Local Moist Processes 2005/ / / /2009 International Polar “Year” (Red)(Blue) Why 3 Field Seasons?: 2006/2007 season is the first field deployment related to the Supersite and will be a shakedown period. Similarly, this is the first field deployment for the U.S. Twin Otter and Aerosondes. Activities will be concentrated near McMurdo (local activities). 2007/2008 season is when local scale studies are expanded to the Ross Ice Shelf and north of Ross Island. 2008/2009 season expands to regional focus. This will be facilitated by the C-130 and HIAPER Hemispheric Interactions

Year:04/0505/0606/0707/0808/0909/? Regional Surface-Based Array – RIME Supersite– Aircraft Studies – Modeling.3.5 Satellite Remote Sensing–.5 – Climate Studies--.5 Support (e.g., RPO mtgs, data mgmt) Total RIME Budget Estimates by Observation Type/Discipline (Estimate in Millions of $) Assumptions: Supersite continuous ops FY07-09 U.S. Twin Otter “provided” by USAP Polar C-130 deployment cost only HIAPER aircraft funneled through NSF deployment pool 2009/10 and later resources for analysis activities Current Funding: Parish and Cassano: RAS Study ~150 K/y Kuo et al. – Data Assimilation ~250 K/y

Discussion Topics The likely future funding profile for the RIME project. As we have seen, the project requires resources far in excess of the normal budget for Polar Oceans and Climate Systems. Consideration of submission deadline delay for RIME proposals (July 1, 2004)? What is the best way to coordinate proposals? Are individual or collaborative approaches preferred? Discussion of aircraft platform requirements for RIME. Building and maintaining the Supersite. Need for RIME-SMO (RIME Science Management Office) and responsibilities. Intl collaborations, (e.g., UK, Italy, etc), to improve RIME observational network and help answer key science questions.