Suck. Swallow. Breathe.

Video, Dur: 7 min, HD DVC Pro 2009 Based on the principle of assembling a series of improvised acts, the performance is driven by a concern for the image, sound and gesture and the staging of both contemplative and active human presences. Featuring a woman and child duo the video performs the élan vital within a fairytale scenery.

WE

Inspired by the dystopian fiction of Yevgeny Zamyatin and the minimal synthesiser music of the early 80s, London-based artist duo Pil and Galia Kollectiv are joined by Victor M. Jakeman and Ruth Angel Edwards to present popular chart hits in new versions, turning songs about 'me' and 'you' into songs about 'us', and replacing the individual 'I' with the collective 'WE'. The performance WE reveals the latent politics of the love song by annihilating its liberal subject; through the simple substitution of the plural for the singular, intimacy becomes a form of collective action and the unique the universal. Sonically, WE follows in the footsteps of bands like The Better Beatles, who sought to improve on the canon of popular music by stripping it bare, even. WE, performed at Kunsthall Oslo, Royal Standard Liverpool and ICA London, is also released on a 10" vinyl record and accompanied by a music video commissioned by Tate Britain for Tate Shots.

Wind observations above an urban river using a new lidar technique, scintillometry and anemometry

Flow along rivers, an integral part of many cities, might provide a key mechanism for ventilation – which is important for air quality and heat stress. Since the flow varies in space and time around rivers, there is limited utility in point measurements. Ground-based remote sensing offers the opportunity to study 3D flow in locations which are hard to observe. For three months in the winter and spring of 2011, the atmospheric flow above the River Thames in central London was observed using a scanning Doppler lidar, a dual-beam scintillometer and sonic anemometry. First, an inter-comparison showed that lidar-derived mean wind-speed estimates compare almost as well to sonic anemometers (root-mean-square error (rmse) 0.65–0.68 m s–1) as comparisons between sonic anemometers (0.35–0.73 m s–1). Second, the lidar duo-beam scanning strategy provided horizontal transects of wind vectors comparison with scintillometer rmse 1.12–1.63 m s–1) which revealed mean and turbulent flow across the river and surrounds; in particular: chanelling flow along the river and turbulence changes consistent with the roughness changes between built to river environments. The results have important consequences for air quality and dispersion around urban rivers, especially given that many cities have high traffic rates on bankside roads.

Separating the influence of projected changes in air temperature and wind on patterns of sea level change and ocean heat content

We present ocean model sensitivity experiments aimed at separating the influence of the projected changes in the “thermal” (near-surface air temperature) and “wind” (near-surface winds) forcing on the patterns of sea level and ocean heat content. In the North Atlantic, the distribution of sea level change is more due to the “thermal” forcing, whereas it is more due to the “wind” forcing in the North Pacific; in the Southern Ocean, the “thermal” and “wind” forcing have a comparable influence. In the ocean adjacent to Antarctica the “thermal” forcing leads to an inflow of warmer waters on the continental shelves, which is somewhat attenuated by the “wind” forcing. The structure of the vertically integrated heat uptake is set by different processes at low and high latitudes: at low latitudes it is dominated by the heat transport convergence, whereas at high latitudes it represents a small residual of changes in the surface flux and advection of heat. The structure of the horizontally integrated heat content tendency is set by the increase of downward heat flux by the mean circulation and comparable decrease of upward heat flux by the subgrid-scale processes; the upward eddy heat flux decreases and increases by almost the same magnitude in response to, respectively, the “thermal” and “wind” forcing. Regionally, the surface heat loss and deep convection weaken in the Labrador Sea, but intensify in the Greenland Sea in the region of sea ice retreat. The enhanced heat flux anomaly in the subpolar Atlantic is mainly caused by the “thermal” forcing.

Black Forest Magic

Duo Show: John Russell & Dan Mitchell.