COAPS Virtual Library (Publications)

Latif, M., Anderson, D., Barnett, T., Cane, M., Kleeman, R., Leetmaa, A., et al. (1998). A review of the predictability and prediction of ENSO. J. Geophys. Res., 103(C7), 14375–14393. https://www.coaps.fsu.edu/bibliography/show.php?record=746
Bourassa, M. A., Freilich, M. H., Legler, D. M., Liu, W. T., & O'Brien, J. J. (1997). Wind observations from new satellite and research vessels agree (Vol. 78). https://www.coaps.fsu.edu/bibliography/show.php?record=726
Meyers, S. D., & O'Brien, J. J. (1995). Pacific Ocean influences atmospheric carbon dioxide. Eos Trans. AGU, 76(52), 533. https://www.coaps.fsu.edu/bibliography/show.php?record=716
Xu, X., Bower, A., Furey, H., & Chassignet, E. P. (2018). Variability of the Iceland-Scotland Overflow Water Transport Through the Charlie-Gibbs Fracture Zone: Results From an Eddying Simulation and Observations. J. Geophys. Res. Oceans, 123(8), 5808–5823. Abstract: Observations show that the westward transport of the Iceland‐Scotland overflow water (ISOW) through the Charlie‐Gibbs Fracture Zone (CGFZ) is highly variable. This study examines (a) where this variability comes from and (b) how it is related to the variability of ISOW transport at upstream locations in the Iceland Basin and other ISOW flow pathways. The analyses are based on a 35‐year 1/12° eddying Atlantic simulation that represents well the main features of the observed ISOW in the area of interest, in particular, the transport variability through the CGFZ. The results show that (a) the variability of the ISOW transport is closely correlated with that of the barotropic transports in the CGFZ associated with the meridional displacement of the North Atlantic Current front and is possibly induced by fluctuations of large‐scale zonal wind stress in the Western European Basin east of the CGFZ; (b) the variability of the ISOW transport is increased by a factor of 3 from the northern part of the Iceland Basin to the CGFZ region and transport time series at these two locations are not correlated, further suggesting that the variability at the CGFZ does not come from the upstream source; and (c) the variability of the ISOW transport at the CGFZ is strongly anticorrelated to that of the southward ISOW transport along the eastern flank of the Mid‐Atlantic Ridge, suggesting an out‐of‐phase covarying transport between these two ISOW pathways. Keywords: Iceland; Scotland overflow water; Charlie; Gibbs fracture zone; variability; volume transport; eddying simulation https://www.coaps.fsu.edu/bibliography/show.php?record=952
Winterbottom, H. R., Uhlhorn, E. W., & Chassignet, E. P. (2012). A design and an application of a regional coupled atmosphere-ocean model for tropical cyclone prediction. J. Adv. Model. Earth Syst., 4(4). https://www.coaps.fsu.edu/bibliography/show.php?record=237
DiNapoli, S. M., & Misra, V. (2012). Reconstructing the 20th century high-resolution climate of the southeastern United States. J. Geophys. Res., 117(D19), n/a-n/a. https://www.coaps.fsu.edu/bibliography/show.php?record=238
Yu, L., & Jin, X. (2012). Buoy perspective of a high-resolution global ocean vector wind analysis constructed from passive radiometers and active scatterometers (1987-present). J. Geophys. Res., 117(C11). Keywords: OAFlux; ocean vector; satellite-based; wind analysis https://www.coaps.fsu.edu/bibliography/show.php?record=272
Holthuijsen, L. H., Powell, M. D., & Pietrzak, J. D. (2012). Wind and waves in extreme hurricanes. J. Geophys. Res., 117(C9), n/a-n/a. Keywords: GPS sondes; hurricanes; swell; wave breaking; white caps; wind drag https://www.coaps.fsu.edu/bibliography/show.php?record=268
Nyadjro, E. S., Subrahmanyam, B., Murty, V. S. N., & Shriver, J. F. (2012). The role of salinity on the dynamics of the Arabian Sea mini warm pool. J. Geophys. Res., 117(C9), n/a-n/a. Keywords: Arabian Sea; Argo; HYCOM; SMOS; salinity; warm pool https://www.coaps.fsu.edu/bibliography/show.php?record=271
Winterbottom, H. R., & Chassignet, E. P. (2011). A vortex isolation and removal algorithm for numerical weather prediction model tropical cyclone applications. J. Adv. Model. Earth Syst., 3(4). https://www.coaps.fsu.edu/bibliography/show.php?record=313

Abstract: Observations show that the westward transport of the Iceland‐Scotland overflow water (ISOW) through the Charlie‐Gibbs Fracture Zone (CGFZ) is highly variable. This study examines (a) where this variability comes from and (b) how it is related to the variability of ISOW transport at upstream locations in the Iceland Basin and other ISOW flow pathways. The analyses are based on a 35‐year 1/12° eddying Atlantic simulation that represents well the main features of the observed ISOW in the area of interest, in particular, the transport variability through the CGFZ. The results show that (a) the variability of the ISOW transport is closely correlated with that of the barotropic transports in the CGFZ associated with the meridional displacement of the North Atlantic Current front and is possibly induced by fluctuations of large‐scale zonal wind stress in the Western European Basin east of the CGFZ; (b) the variability of the ISOW transport is increased by a factor of 3 from the northern part of the Iceland Basin to the CGFZ region and transport time series at these two locations are not correlated, further suggesting that the variability at the CGFZ does not come from the upstream source; and (c) the variability of the ISOW transport at the CGFZ is strongly anticorrelated to that of the southward ISOW transport along the eastern flank of the Mid‐Atlantic Ridge, suggesting an out‐of‐phase covarying transport between these two ISOW pathways.

Keywords: Iceland; Scotland overflow water; Charlie; Gibbs fracture zone; variability; volume transport; eddying simulation

https://www.coaps.fsu.edu/bibliography/show.php?record=952

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