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    A series of uncoupled stand-alone atmosphere and ocean model simulations are performed to investigate the cause of the coupled model bias.(HINT: you don't even need a web site to get a free Para Chat room.) I'd rather pay a reasonable fee for more features and no advertisements. Para Chat offers full-featured, ad-free services for personal, small business and enterprise web sites.You can try them for free right now on your own web site!Each choice of view option allows for a different screen configuration.I'm writing a flex 4.5 application that's supposed to capture a video from a webcam and audio from microphone and save it in some video format (i don't care which format). You can check with the red5Recorder which is a player built using flex builder and configurable to any recorder like Red5 server or Flash FMS.You will see the entry on your chat credit history as "Revenue Share The chat app provides an excellent use of screen area for the many functionalities.You may choose to view in portrait or landscape mode.Consequently, this contributes to the warm SST bias in the ABFZ by 2 °C (compared to the reanalysis forced simulation).There is no evidence that local air-sea feedbacks among wind stress curl, SST, and sea level pressure (SLP) affect the ABFZ SST bias. Our chat room is one of the busiest chat rooms on the chat service.When you login you have the option to chat randomly with many people from all over the world using a cam, mic and text.The stand-alone atmosphere model driven with observed SST exhibits a similar cyclonic surface circulation bias; while the stand-alone ocean model forced with the reanalysis data produces a warm SST in the ABFZ with a magnitude approximately half of that in the coupled Nor ESM simulation.An additional uncoupled sensitivity experiment shows that the atmospheric model’s local negative surface wind curl generates anomalously strong Angola Current at the ocean surface.Turbulent surface heat flux differences between coupled and uncoupled experiments explain the remaining 2 °C warm SST bias in Nor ESM.

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