Impact of Usage of Multiple-Satellite Sensors on Accuracy of Sea Surface Wind Data

Author(s):  
Ayumi Koizumi ◽  
Masahisa Kubota ◽  
Kunio Kutsuwada
2019 ◽  
Vol 41 (15) ◽  
pp. 5770-5784 ◽  
Author(s):  
Ayumi Koizumi ◽  
Masahisa Kubota ◽  
Kunio Kutsuwada ◽  
Tsutomu Hihara ◽  
Hiroyuki Tomita

Author(s):  
Felix R. Rodriguez ◽  
Daniel Teomiro Villa ◽  
Jaime Pina Cambero ◽  
Diego J. Merino Fernandez

2014 ◽  
Vol 9 (2) ◽  
pp. 192-201 ◽  
Author(s):  
Yi Yu ◽  
Weimin Zhang ◽  
Zhongyuan Wu ◽  
Xiaofeng Yang ◽  
Xiaoqun Cao ◽  
...  

2003 ◽  
Vol 12 (6) ◽  
pp. 551-563 ◽  
Author(s):  
Masahisa KUBOTA ◽  
Daisuke MINAMI ◽  
Takashi Ooki ◽  
Sou Suzuki

2020 ◽  
Vol 7 (4) ◽  
pp. 233-241
Author(s):  
Donghwi Son ◽  
Kicheon Jun ◽  
Jae-Seol Shim ◽  
Jae-il Kown ◽  
Jeseon Yoo

2012 ◽  
Vol 50 (7) ◽  
pp. 2901-2909 ◽  
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Alexis A. Mouche ◽  
Fabrice Collard ◽  
Bertrand Chapron ◽  
Knut-Frode Dagestad ◽  
Gilles Guitton ◽  
...  

2019 ◽  
Vol 11 (9) ◽  
pp. 1112
Author(s):  
Guoqing Han ◽  
Changming Dong ◽  
Junde Li ◽  
Jingsong Yang ◽  
Qingyue Wang ◽  
...  

Based on both satellite remote sensing sea surface temperature (SST) data and numerical model results, SST warming differences in the Mozambique Channel (MC) west of the Madagascar Island (MI) were found with respect to the SST east of the MI along the same latitude. The mean SST west of the MI is up to about 3.0 °C warmer than that east of the MI. The SST differences exist all year round and the maximum value appears in October. The area of the highest SST is located in the northern part of the MC. Potential factors causing the SST anomalies could be sea surface wind, heat flux and oceanic flow advection. The presence of the MI results in weakening wind in the MC and in turn causes weakening of the mixing in the upper oceans, thus the surface mixed layer depth becomes shallower. There is more precipitation on the east of the MI than that inside the MC because of the orographic effects. Different precipitation patterns and types of clouds result in different solar radiant heat fluxes across both sides of the MI. Warm water advected from the equatorial area also contribute to the SST warm anomalies.


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