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Osada, H. Clausen, C. Hammer, and H. Shoji [27] 1. Assume the density of the sample solution is the , A century comparison of prominent bipolar volcanic events in same as that of water, i.

Legrand, M. Wagenbach , Impact of Cerro Hudson and water equivalent, and 0. Mayewski, P. Lyons, M. Spencer, M. Twickler, C. Buck, [29] 3. Meeker, M. Morrison, M. Twickler, S. Ferland, D. Meese, M. Legrand, and J. Monzier, M. Robin, and J. We thank all the scientists who have sup- forgotten caldera, J. Narita, and N.

Maeno , A continuous — year analyzing the cores and for allowing us to use them. We thank Philippe record of volcanic activity from East Antarctica, J. This work is 17, — 17, Thompson, J. Dai, M. Davis, and P. Mosley-Thompson, E. Mashiotta, and L. Wagenbach, H. Fischer, J. Kipfstuhl, H. Millar, S. Oppenheimer, core over the last years based on continuous flow analysis, Ann. Naveau, P. Ammann, H. Oh, and W. Oerter, H. Fischer, R. Weller, and H. Miller , Spatio- Atmosphere, Geophys.

Robock and temporal variability in volcanic sulphate deposition over the past 2kyr in C. Morgan, A. Curran, T. Van Ommen, and P. AGU, 74, Zielinski, G. Mayewski, L. Meeker, S. Whitlow, M. Twickler, Robock, A. Free , Ice cores as an index of global volcan- M. Morrison, D. Meese, A. Gow, and R. Alley , Record ism from 1 to the present, J. Free , The volcanic record in ice cores for the implications for the volcano-climate system, Science, , — Dibb, Q.

Yang, P. Whitlow, and M. Last Years, edited by P. Jones, R. Bradley, and J. Jouzel, pp. World, 47, 8 — Simkin, T. Siebert , Volcanoes of the World, pp. Appenzeller, R. Rothlisberger, M. Hutterli, B. Oerter, F. Wilhelms, D. Miller, and R. Mulvaney C. Gao and A. Wagenbach, R. Mulvaney, and H. Fischer b , Glacio- P. Maud Land, Antarctica: 2. Seasonally resolved chemical records, J. Geo- S. Stenchikov, G. Kirchner, A. Robock, H. Graf, J. Siggaard-Andersen, and S. Johnsen, Grainger, A.

Lambert, and L. Proposito, R. Gragnani, O. Flora, J. Jouzel, S. Both regions produce their effect primarily by altering wave propagation and angular momentum transports, but planetary wave energy changes accompanying tropospheric climate change are also important. Stratospheric forcing has a larger impact on the NAO than on the AO, and the angular momentum transport changes associated with it peak in the upper troposphere, affecting all wavenumbers.

Tropospheric climate changes influence both the AO and NAO with effects that extend throughout the troposphere. For both forcings there is often vertical consistency in the sign of the momentum transport changes, obscuring the difference between direct and indirect mechanisms for influencing the surface circulation.

Publication Abstracts Rind et al. Learn more and set cookies Close. Ponce, Manuel Connect to add to a playlist Added the Dobrinescu, Ioan Connect to add to a playlist Added the Many of his compositions are strongly influenced by the harmonies and form of traditional songs. Estrelkita wrote music for solo instruments, chamber ensembles, and orchestra.

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