Abstract We report on a measurement of Spin Density Matrix Elements (SDMEs) in hard exclusive$$\rho ^0$$ meson muoproduction at COMPASS using 160 GeV/cpolarised$$ \mu ^{+}$$ and$$ \mu ^{-}$$ beams impinging on a liquid hydrogen target. The measurement covers the kinematic range 5.0 GeV/$$c^2$$ $$< W<$$ 17.0 GeV/$$c^2$$ , 1.0 (GeV/c)$$^2$$ $$< Q^2<$$ 10.0 (GeV/c)$$^2$$ and 0.01 (GeV/c)$$^2$$ $$< p_{\textrm{T}}^2<$$ 0.5 (GeV/c)$$^2$$ . Here,Wdenotes the mass of the final hadronic system,$$Q^2$$ the virtuality of the exchanged photon, and$$p_{\textrm{T}}$$ the transverse momentum of the$$\rho ^0$$ meson with respect to the virtual-photon direction. The measured non-zero SDMEs for the transitions of transversely polarised virtual photons to longitudinally polarised vector mesons ($$\gamma ^*_T \rightarrow V^{ }_L$$ ) indicate a violation ofs-channel helicity conservation. Additionally, we observe a dominant contribution of natural-parity-exchange transitions and a very small contribution of unnatural-parity-exchange transitions, which is compatible with zero within experimental uncertainties. The results provide important input for modelling Generalised Parton Distributions (GPDs). In particular, they may allow one to evaluate in a model-dependent way the role of parton helicity-flip GPDs in exclusive$$\rho ^0$$ production. 
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                            Field measurements of turbulent mixing south of the Lombok Strait, Indonesia
                        
                    
    
            Abstract The Indonesian seas, with their complex passages and vigorous mixing, constitute the only route and are critical in regulating Pacific–Indian Ocean interchange, air–sea interaction, and global climate events. Previous research employing remote sensing and numerical simulations strongly suggested that this mixing is tidally driven and localized in narrow channels and straits, with only a few direct observations to validate it. The current study offers the first comprehensive temporal microstructure observations in the south of Lombok Strait with a radius of 0.05° and centered on 115.54oE and 9.02oS. Fifteen days of tidal mixing observations measured potential temperature and density, salinity, and turbulent energy dissipation rate. The results revealed significant mixing and verified the remotely sensed technique. The south Lombok temporal and depth averaged of the turbulent kinetic energy dissipation rate, and the diapycnal diffusivity from 20 to 250 m are$$\varepsilon$$  = 4.15 ± 15.9) × 10–6W kg–1and$$K\rho$$ = (1.44 ± 10.7) × 10–2m2s–1, respectively. This$$K\rho$$ is up to 104times larger than the Banda Sea [$$K\rho$$  = (9.2 ± 0.55) × 10–6m2s–1] (Alford et al. Geophys Res Lett 26:2741–2744, 1999) or the “open ocean”$$K\rho$$ = 0.03 × 10–4 m2s−1within 2° of the equator to (0.4–0.5) × 10–4m2s−1at 50°–70° (Kunze et al. J Phys Oceanogr 36:1553–1576, 2006). Therefore, nonlinear interactions between internal tides, tidally induced mixing, and ITF plays a critical role regulating water mass transformation and have strong implications to longer-term variations and change of Pacific–Indian Ocean water circulation and climate. 
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                            - Award ID(s):
- 2242151
- PAR ID:
- 10533232
- Publisher / Repository:
- Springer Science + Business Media
- Date Published:
- Journal Name:
- Geoscience Letters
- Volume:
- 11
- Issue:
- 1
- ISSN:
- 2196-4092
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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