Articles | Volume 1, issue 2
Weather Clim. Dynam., 1, 701–713, 2020
Weather Clim. Dynam., 1, 701–713, 2020

Research article 10 Nov 2020

Research article | 10 Nov 2020

The role of heat-flux–temperature covariance in the evolution of weather systems

Andrea Marcheggiani and Maarten H. P. Ambaum

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Cited articles

Ambaum, M. H. and Novak, L.: A nonlinear oscillator describing storm track variability, Q. J. Roy. Meteorol. Soc., 140, 2680–2684, 2014. a, b, c, d, e, f, g
Athanasiadis, P. J. and Ambaum, M. H. P.: Linear Contributions of Different Time Scales to Teleconnectivity, J. Climate, 22, 3720–3728,, 2009. a
Blackmon, M. L., Wallace, J. M., Lau, N.-C., and Mullen, S. L.: An observational study of the Northern Hemisphere wintertime circulation, J. Atmos. Sci., 34, 1040–1053, 1977. a
Chang, E. K. and Zurita-Gotor, P.: Simulating the seasonal cycle of the Northern Hemisphere storm tracks using idealized nonlinear storm-track models, J. Atmos. Sci., 64, 2309–2331, 2007. a, b
Chang, E. K., Lee, S., and Swanson, K. L.: Storm track dynamics, J. Climate, 15, 2163–2183, 2002. a, b, c, d, e
Short summary
In this paper, we investigate air–sea interaction by looking at the relationship between spatial variability in surface heat flux and air temperature. We observe that their interaction characterises different stages of storm evolution, thus providing a new perspective on the role played by air–sea heat exchange.