V. Righi, M. Starkey , G. Dai, L. G. Rahme, and A. A. Tzika NMR Surgical Laboratory, Department of Surgery, Massachusetts General Hospital and Shriners Burns Institute, Harvard Medical School, Boston, MA, United States, Department of Radiology, Massachusetts General Hospital, Harvard Medical School, Athinoula A. Martinos Center for Biomedical Imaging, Boston, MA, United States, Molecular Surger...

D. Mintzopoulos, L. G. Astrakas, G. C. Wiggins, L. L. Wald, B. R. Rosen, and A. A. Tzika NMR Surgical Laboratory, Department of Surgery, and Shriners Burn Institute, Massachusetts General Hospital, Boston, MA, United States, Athinoula A. Martinos Center for Biomedical Imaging, Massachusetts General Hospital, Boston, MA, United States, Athinoula A. Martinos Center for Biomedical Imaging and Dept...

O. D. Miller, C. W. Hsu, 3 M. T. H. Reid, W. Qiu, B. G. DeLacy, J. D. Joannopoulos, M. Soljačić, and S. G. Johnson Department of Mathematics, Massachusetts Institute of Technology, Cambridge, MA 02139 Department of Physics, Massachusetts Institute of Technology, Cambridge, MA 02139 Department of Physics, Harvard University, Cambridge, MA 02138 U.S. Army Edgewood Chemical Biological Center, Rese...

C. Catana, A. van der Kouwe, T. Benner, M. Hamm, B. Guerin, L. Byars, C. Michel, G. El Fakhri, M. Schmand, B. R. Rosen, and A. G. Sorensen MGH, Radiology, A.A. Martinos Center for Biomedical Imaging, Charlestown, MA, United States, Siemens Medical Solutions USA Inc., Charlestown, MA, United States, Nuclear Medicine and Molecular Imaging, Massachusetts General Hospital, Boston, MA, United States...

The objective of this work is to compare various ET models based on a standard dataset. We selected 9 ET models for comparison, including three surface energy balance residual models (SEBS, TSEB-P and TSEB-S), four Penman-Monteith models (PM-Mu, PM-Yuan, PM-Sun and PM-SW), one Priestly-Taylor model (PT-Fi) and one semi-empirical statiacital model (ST). ET is evaluated using surface climate data...

The Weishan Irrigation Zone along the lower reaches of the Yellow River consists of a total irrigated area of 3600 ha. The region has an average annual rainfall of 500–600 mm, with 60–70% of local rainfall occurring during the summer, and with less than 15% in spring. The water deficit during the spring affects the winter wheat growth from March to early June, which is a major growth period sig...