Author  |
Title |
Year |
Publication |
Volume |
Pages |
Misra, V.; Li, H. |
The seasonal climate predictability of the Atlantic Warm Pool and its teleconnections |
2014 |
Geophysical Research Letters |
41 |
661-666 |
Misra, V.; Li, H.; Kozar, M. |
The precursors in the Intra-Americas Seas to seasonal climate variations over North America |
2014 |
Journal of Geophysical Research: Oceans |
119 |
2938-2948 |
Misra, V.; Li, H.; Wu, Z.; DiNapoli, S. |
Global seasonal climate predictability in a two tiered forecast system: part I: boreal summer and fall seasons |
2014 |
Climate Dynamics |
42 |
1425-1448 |
Nag, B.; Misra, V.; Bastola, S. |
Validating ENSO Teleconnections on Southeastern U.S. Winter Hydrology |
2014 |
Earth Interactions |
18 |
1-23 |
Nedbor-Gross, R.; Dukhovskoy, D.S.; Bourassa, M.A.; Morey, S.L.; Chassignet, E.P. |
Investigation of the Relationship Between the Yucatan Channel Transport and the Loop Current Area in a Multidecadal Numerical Simulation |
2014 |
Marine Technology Society Journal |
48 |
15-26 |
Nguyen, T. T. |
Variability of Cross-Slope Flow in the Desoto Canyon Region |
2014 |
|
|
|
Oh, J.-H.; Shin, D.W.; Cocke, S.D.; Baigorria, G.A. |
ENSO Teleconnection Pattern Changes over the Southeastern United States under a Climate Change Scenario in CMIP5 Models |
2014 |
Advances in Meteorology |
|
1-16 |
Purna Chand, C.; Rao, M.V.; Ramana, I.V.; Ali, M.M.; Patoux, J.; Bourassa, M.A. |
Estimation of sea level pressure fields during Cyclone Nilam from Oceansat-2 scatterometer winds |
2014 |
Atmospheric Science Letters |
15 |
65-71 |
Seitz, C. |
Estimating the Effects of Climate Change on Tropical Cyclone Activity |
2014 |
|
|
|
Shaevitz, D.A.; Camargo, S.J.; Sobel, A.H.; Jonas, J.A.; Kim, D.; Kumar, A.; LaRow, T.E.; Lim, Y.-K.; Murakami, H.; Reed, K.A.; Roberts, M.J.; Scoccimarro, E.; Vidale, P.L.; Wang, H.; Wehner, M.F.; Zhao, M.; Henderson, N. |
Characteristics of tropical cyclones in high-resolution models in the present climate |
2014 |
Journal of Advances in Modeling Earth Systems |
6 |
1154-1172 |