ON THE ORIGIN OF MID-LATITUDE FAST WIND: CHALLENGING THE TWO-STATE SOLAR WIND PARADIGM by Stakhiv, Mark, Landi, Enrico, Lepri, Susan T., Oran, Rona, Zurbuchen, Thomas H.

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Workshop on Climate Effects of Wind Turbines by Hoss, Frauke, Keith, David, Kuang, Zhiming, Lundquist, Julie, Miller, Lee, Emanuel, Kerry Andrew

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On the Wind Power Input to the Ocean General Circulation by Zhai, Xiaoming, Johnson, Helen L., Marshall, David P., Wunsch, Carl Isaac

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On the Patterns of Wind-Power Input to the Ocean Circulation by Roquet, Fabien, Madec, Gurvan, Wunsch, Carl Isaac

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Predictability of SST-Modulated Westerly Wind Bursts by Tziperman, Eli, Gebbie, Geoffrey

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Agents of seed dispersal : animal--zoochary / Wind--anemonochory by Lysakowski, Lukasz Kamil, 1974-

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The Global Characteristics of the Wavenumber Spectrum of Ocean Surface Wind by Xu, Yongsheng, Fu, Lee-Lueng, Tulloch, Ross

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The Dynamics of Mesoscale Winds in the Upper Troposphere and Lower Stratosphere by Bühler, Oliver, Callies, Joern, Ferrari, Raffaele

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The Dependence of Southern Ocean Meridional Overturning on Wind Stress by Abernathey, Ryan Patrick, Ferreira, David, Marshall, John C

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TRANSPORT OF THE FIRST ROCKS OF THE SOLAR SYSTEM BY X-WINDS by Hu, Renyu

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Potential Impacts of Offshore Wind Farms on North Sea Stratification by Carpenter, Jeffrey R., Merckelbach, Lucas, Callies, Ulrich, Clark, Suzanna, Gaslikova, Lidia, Baschek, Burkard

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Buoyancy and Wind-Driven Convection at Mixed Layer Density Fronts by Taylor, John Ryan, Ferrari, Raffaele

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ON SUN-TO-EARTH PROPAGATION OF CORONAL MASS EJECTIONS: II. SLOW EVENTS AND COMPARISON WITH OTHERS by Liu, Ying D., Hu, Huidong, Luhmann, Janet G., Yang, Zhongwei, Wang, Rui, Wang, Chi, 1967-, Richardson, John D.

“…We compare slow CMEs with fast and intermediate-speed events, and obtain key results complementing the attempt of Liu et al. to create a general picture of CME Sun-to-Earth propagation: (1) the Sun-to-Earth propagation of a typical slow CME can be approximately described by two phases, a gradual acceleration out to about 20–30 solar radii, followed by a nearly invariant speed around the average solar wind level; (2) comparison between different types of CMEs indicates that faster CMEs tend to accelerate and decelerate more rapidly and have shorter cessation distances for the acceleration and deceleration; (3) both intermediate-speed and slow CMEs would have speeds comparable to the average solar wind level before reaching 1 au; (4) slow CMEs have a high potential to interact with other solar wind structures in the Sun–Earth space due to their slow motion, providing critical ingredients to enhance space weather; and (5) the slow CMEs studied here lack strong magnetic fields at the Earth but tend to preserve a flux-rope structure with an axis generally perpendicular to the radial direction from the Sun. …”
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Rapid changes in mixed layer stratification driven by submesoscale instabilities and winds by Ferrari, Raffaele, Tandon, A., Mahadevan, Amala

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Simulated Response of the Arctic Freshwater Budget to Extreme NAO Wind Forcing by Condron, Alan, Winsor, Peter, Hill, Christopher N., Menemenlis, Dimitris

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Eddy Transport and Mixing in a Wind- and Buoyancy-Driven Jet on the Sphere by Cerovecki, Ivana, Plumb, R. Alan, Heres, William

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On the Variability of Wind Power Input to the Oceans with a Focus on the Subpolar North Atlantic by Zhai, Xiaoming, Wunsch, Carl Isaac

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On the Relationship between SST Gradients, Boundary Layer Winds, and Convergence over the Tropical Oceans by Back, Larissa E., Bretherton, Christopher S.

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Robust Wind and Precipitation Responses to the Mount Pinatubo Eruption, as Simulated in the CMIP5 Models by Barnes, Elizabeth A., Solomon, Susan, Polvani, Lorenzo M.

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On the climate variability of tropical cyclone potential intensity and Atlantic hurricane activity by Rousseau-Rizzi, Raphaël

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