Historical trends in the jet streams Cristina Archer and Ken Caldeira Department of Global Ecology Carnegie Institution for Science Cristina Archer and.

Slides:



Advertisements
Similar presentations
Simulated and observed geopotential height and temperature changes.
Advertisements

Class #5: Air pressure and winds Chapter 8 1Class #5 Tuesday, July 13, 2010.
Annular Modes of Extra- tropical Circulation Judith Perlwitz CIRES-CDC, University of Colorado.
Mrs. Wharton’s Science Class
Unit 9: Circulation Patterns of the Atmosphere
Aim: What are some of Earth’s wind patterns? I. Winds and Pressure Belts A. Convection cell – when air circulates by rising in one place and sinking at.
Eddy-Zonal Flow Feedback in the Southern and Northern Hemispheres A Review of Two Papers by D. J. Lorenz and D. L. Hartmann Stephanie Sydorko AT750.
Ice-Atmosphere Interaction (2): Melting of Greenland Ice Sheet By: Eric DoBroka.
Spring Onset in the Northern Hemisphere: A Role for the Stratosphere? Robert X. Black Brent A. McDaniel School of Earth and Atmospheric Sciences Georgia.
Is Arctic Warming Causing Extremes in Mid-Latitude Weather? Florence Chen, Joseph Lanzillo, Upasna Sharma.
General circulation in the tropics
1 Trade Winds in Equatorial Pacific. 2 ITCZ Location July January ITCZ.
Lessons 22,23,24 Upper Level Winds
MGS Accelerometer-derived profiles of Upper Atmospheric Pressures and Temperatures: Similarities, Differences, and Winds Withers, Bougher, and Keating.
GLOBAL CHANGES IN OUR ATMOSPHERE: a top-down point of view  Atmospheric Science 101  Structure of atmosphere  Important relationships  The Northern.
Protecting our Health from Climate Change: a Training Course for Public Health Professionals Chapter 2: Weather, Climate, Climate Variability, and Climate.
Brief Climate Discussion William F. Ryan Department of Meteorology The Pennsylvania State University.
Global Wind Patterns Science Lesson Objectives ► using scientific theory, describe and explain heat transfer and its consequences in both the atmosphere.
UPPER-LEVEL WINDS Atmospheric pressure, temperature and winds at surface.
Class #13 Monday, September 27, 2010 Class #13: Monday, September 27 Chapter 7 Global Winds 1.
Wind Causes of Wind.
Arctic Climate Change John C. Fyfe Canadian Centre for Climate Modelling and Analysis.
PAGE 1 Using millennial AOGCM simulation as a laboratory to derive and test hypotheses Hans von Storch 12, E. Zorita 1 and F. González-Rouco 3 1 Institute.
Drivers of multidecadal variability in JJA ozone concentrations in the eastern United States Lu Shen, Loretta J. Mickley School of Engineering and Applied.
THE 3 CELL MODEL.
1 Hadley Centre The Atlantic Multidecadal Oscillation: A signature of persistent natural thermohaline circulation cycles in observed climate Jeff Knight,
Quasi-stationary planetary wave long-term changes in total ozone over Antarctica and Arctic A.Grytsai, O.Evtushevsky, O. Agapitov, A.Klekociuk, V.Lozitsky,
Benjamin A. Schenkel and Robert E. 4 th WCRP International Conference on Reanalyses Department of Earth, Ocean,
Long-Term Changes in Northern and Southern Annular Modes Part I: Observations Christopher L. Castro AT 750.
Sensitivity of Antarctic climate to the distribution of ozone depletion Nathan Gillett, University of East Anglia Sarah Keeley, University of East Anglia.
Bifurcation Dynamics L. Gourdeau (1), B. Kessler (2) 1), LEGOS/IRD Nouméa, New Caledonia, 2) NOAA/PMEL, Seattle, USA Why is it important to study the bifurcation.
THE ATMOSPHERE. aTMOSPHERIC pRESSURE Air Pressure- the measure of the force with which the air molecules push on a surface. Air pressure changes throughout.
Global Climate Change: Past and Future Le Moyne College Syracuse, New York February 3, 2006 Department of Meteorology and Earth and Environmental Systems.
MET 10 1 The General Circulation of the Atmosphere.
PAPER REVIEW R Kirsten Feng. Impact of global warming on the East Asian winter monsoon revealed by nine coupled atmosphere-ocean GCMs Masatake.
Dynamical Influence on Inter-annual and Decadal Ozone Change Sandip Dhomse, Mark Weber,
Dynamical Impacts of Antarctic Stratospheric Ozone Depletion on the Extratropical Circulation of the Southern Hemisphere Kevin M. Grise David W.J. Thompson.
THE 3 CELL MODEL.
What is Climate Change?. Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words,
The MJO and Arctic Air Temperatures Gabriel A. Vecchi and Nicholas A. Bond JISAO, University of Washington and NOAA/Pacific Marine Environmental Laboratory.
Changes in Sea Ice Alison Liou Meghan Goodwin. Arctic Oscillation (Northern Annular Mode) Antarctic Oscillation (Southern Annular Mode) Zonal = movement.
Day Meridional Propagation of Global Circulation Anomalies ( A Global Convection Circulation Paradigm for the Annular Mode) Ming Cai 1 and R-C.
THE INFLUENCE OF THE 11-YEAR SOLAR CYCLE ON THE STRATOSPHERE BELOW 30KM: A REVIEW H. VAN LOON K. LABITZKE 2010/04/13 Pei-Yu Chueh.
ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE ENVIRONMENTAL SCIENCE TEACHERS’ CONFERENCE, Borki Molo, Poland, 7-10 February 2007 Extreme Climatic and atmospheric.
Class #16 Monday, October 5 Class #16: Monday, October 5 Chapter 7 Global Winds 1.
Weather Lesson Three Wind Belts. CORIOLIS EFFECT Deflection of winds caused by Earth’s rotation. Winds are deflected to the right in the northern hemisphere,
 The horizontal movement of air caused by the uneven heating of the Earths surface.
Makoto INOUE and Masaaki TAKAHASHI (CCSR, Univ. of Tokyo)
METO 637 Lesson 12.
Global Winds What roles do composition, structure, and properties play in our atmosphere?
OCEAN SURFACE CURRENTS
MID-LATITUDE WEATHER SYSTEMS: PART IV: SURFACE-UPPER AIR LINKAGE
Handout (green) Atmospheric Circulation
Question 1 height of the 1000 hPa surface pressure (Pa) at sea level.
Atmospheric Circulation
Global Winds.
The Diurnal Temperature Range and its Recent Evolution
Wind.
Wind Causes of Wind.
Wind Causes of Wind.
Chapter 10 Wind: Global Systems.
Global Winds.
Dynamics of Annular Modes
ExUTLS dynamics and global observations
Sean Davis1,2, Karen Rosenlof1
Weather Notes Part 3.
Wind Causes of Wind.
Global Scale Winds.
THE ATMOSPHERE I CAN EXPLAIN HOW HEAT IS TRANSFERRED IN THE ATMOSPHERE. I CAN DESCRIBE CONDUCTION. I CAN DESCRIBE CONVECTION. I CAN DESCRIBE RADIATION.
Dynamics of Annular Modes
Presentation transcript:

Historical trends in the jet streams Cristina Archer and Ken Caldeira Department of Global Ecology Carnegie Institution for Science Cristina Archer and Ken Caldeira Department of Global Ecology Carnegie Institution for Science AMS Meeting, New Orleans, January 2008

Scientific questions IF, HOW, WHY have the jet streams changed in last decades? Methods  Definition of jet streams  Observed trends  Interpretation Methods  Definition of jet streams  Observed trends  Interpretation Tools Reanalyses (ERA-40 and NCEP/NCAR)

Jet streams: the theory

Jet streams: the reality Koch et al. (2006) Northern Hemisphere Southern Hemisphere

Jet streams: the reality Koch et al. (2006) Northern Hemisphere Southern Hemisphere SpiralAnnular

Jet stream centroids Wind speed Altitude Latitude

Jet stream wind speed

NH SHT SHP

Wind speed trends  NH, SHT weakening  SHP strengthening  NH, SHT weakening  SHP strengthening

Altitude trends  ERA-40: all jets rising significantly  NCEP/NCAR: SHP rising significantly, NH and SHT nearly constant  ERA-40: all jets rising significantly  NCEP/NCAR: SHP rising significantly, NH and SHT nearly constant

Latitude anomaly trends  All jets are moving poleward

Thermal Wind  Zonal wind speed trends similar in both reanalyses  Zonal thermal wind explains partially NH wind speed trends only  Zonal wind speed trends similar in both reanalyses  Zonal thermal wind explains partially NH wind speed trends only

Surface Temperature  Jets rising overall, but more variations in NH  Trends in surface temperature do not explain trends in jet height  Jets rising overall, but more variations in NH  Trends in surface temperature do not explain trends in jet height

Conclusions  Centroid approach to define jet streams  Jet streams have risen in altitude and moved poleward in both hemispheres  NH and SHT jets have weakened, whereas the SHP jet has strengthened  Impact of global warming (via surface temperature) mild in NH jet, not evident in SH jets - HIGHLY SIMPLIFIED APPROACH!  Centroid approach to define jet streams  Jet streams have risen in altitude and moved poleward in both hemispheres  NH and SHT jets have weakened, whereas the SHP jet has strengthened  Impact of global warming (via surface temperature) mild in NH jet, not evident in SH jets - HIGHLY SIMPLIFIED APPROACH!