'Planetary waves' presentation slideshows

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Lecture 9: Air-Sea Interactions

Lecture 9: Air-Sea Interactions

Lecture 9: Air-Sea Interactions. EarthsClimate_Web_Chapter.pdf , p. 22-27; Ch. 16, p. 299-302; Ch. 17, p. 321-324. Geographic Feature of High and Low Pressure Systems. L. L. H. H. H. H. H. L. L. L. L. L. When averaged over time, planetary waves are geographically

By tyne
(162 views)

The coupled stratosphere-troposphere response to impulsive forcing from the troposphere

The coupled stratosphere-troposphere response to impulsive forcing from the troposphere

The coupled stratosphere-troposphere response to impulsive forcing from the troposphere. Thomas J. Reichler Geophysical Fluid Dynamics Laboratory / Princeton University, Princeton NJ Paul J. Kushner Department of Physics / University of Toronto, Toronto Lorenzo M. Polvani

By jebediah
(171 views)

Talk partly based on:

Talk partly based on:

Atmosphere C oupling and Implications for Upper A tmosphere Predictability Han-Li Liu High Altitude Observatory National Center for Atmospheric Research. Talk partly based on:

By dava
(102 views)

Solar Variability and Climate: From Mechanisms to Models

Solar Variability and Climate: From Mechanisms to Models

Solar Variability and Climate: From Mechanisms to Models. Terry Nathan Atmospheric Science Program University of California, Davis. OUTLINE SUN-CLIMATE CONNECTIONS CHALLENGES 11-YEAR SOLAR FORCING KEY CIRCULATION COMPONENTS OF CLIMATE SYSTEM SOLAR VARIABILITY, OZONE AND WAVES

By selia
(107 views)

How satellites have improved our knowledge of planetary waves in the ocean

How satellites have improved our knowledge of planetary waves in the ocean

How satellites have improved our knowledge of planetary waves in the ocean. Paolo Cipollini National Oceanography Centre, Southampton cipo@noc.soton.ac.uk. Schematic of a 1st mode Baroclinic planetary wave. Overview What we knew before altimetry Altimeter-based observations

By marly
(102 views)

Solar Semidiurnal Tide in the Atmosphere

Solar Semidiurnal Tide in the Atmosphere

Solar Semidiurnal Tide in the Atmosphere. Jeff Forbes Department of Aerospace Engineering Sciences University of Colorado, Boulder, CO 80309-0429. Forcing of the Semidiurnal Tide Vertical Propagation of the Semidiurnal Tide and its Interactions with the Overlying Atmosphere

By yelena
(142 views)

Charlotte Pascoe

Charlotte Pascoe

The Quasi Biennial Oscillation Examining the link between equatorial winds and the flow regime of the wintertime polar stratosphere. Charlotte Pascoe. Layout of Talk. Introduction QBO history How does the QBO work? Why is the QBO important? Polar vortex and planetary waves

By joelle
(104 views)

Multivariate Time Series Analysis

Multivariate Time Series Analysis

Multivariate Time Series Analysis. Charles D. Camp MSRI July 18, 2008. PCA: 2 variable example. Weakly Correlated Variables. Strongly Correlated Variables. PCA algorithm. PCA algorithm, cont. PCA algorithm, cont. An example using Column Ozone Data.

By lacy
(116 views)

REFERENCES

REFERENCES

CONTACT DETAILS contact: wright@atm.ox.ac.uk Atmospheric, Oceanic and Planetary Physics, Clarendon Laboratory, Parks Road, Oxford OX1 3PU, UK All results based on HIRDLS v2.04.19 (V004). REFERENCES

By makan
(114 views)

Observations of Gravity Waves in HIRDLS Data

Observations of Gravity Waves in HIRDLS Data

Observations of Gravity Waves in HIRDLS Data. Xiuping Yan, Neil Arnold, John Remedios EOS & RSPP, Department of Physics & Astronomy University of Leicester 26/6/2008. Contents. Motivation What are gravity waves? Why are gravity waves important? Gravity waves in the atmosphere

By dugan
(174 views)

Dynamical balances and tropical stratospheric upwelling

Dynamical balances and tropical stratospheric upwelling

Bill Randel and Rolando Garcia NCAR. Dynamical balances and tropical stratospheric upwelling. Thanks to: Qiang Fu, Andrew Gettelman, Rei Ueyama, Mike Wallace, plus WACCM group at NCAR. Background:.

By xanthus-chandler
(67 views)

T he  V orticity  E quation for a Homogeneous Fluid with Applications

T he V orticity E quation for a Homogeneous Fluid with Applications

Chapter 6. T he V orticity E quation for a Homogeneous Fluid with Applications. The vorticity equation for a layer of homogeneous fluid of variable depth H(x,y). H(x,y). X body force per unit mass. horizontal momentum equations. Cross-differentiation. Continuity equation.

By ashleyjmarshall
(0 views)


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