1 / 14

Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO

Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO. Pascal Terray , 2010. R98229029 陳漢卿. Numerous studies have documented the significant influence of ENSO on climate variability in the Southern hemisphere.

kin
Download Presentation

Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO Pascal Terray, 2010 R98229029 陳漢卿

  2. Numerous studies have documented the significant influence of ENSO on climate variability in the Southern hemisphere. (Karoly 1989; Kidson and Renwick 2002; Trenberth et al. 2002; Carleton 2003) • Some indicate that ENSO are influenced by Antarctic Circumpolar Wave(ACW) or the Southern Annular Mode (SAM). (Van Loon and Shea 1987; Peterson and White 1998; White et al. 2002; White and Annis 2004)

  3. The associated EOF modes can be regarded as the regional expression of a global-scale Southern Hemisphere mode of variability.

  4. Indian Ocean Atlantic Ocean Surface latent heat, Cloudiness, wind-induced mixing

  5. Kelvin wave

  6. Sets the stage for deep convection by destabilizing the vertical structure of the atmosphere (e.g. due to the increased vertical temperature gradient) • Decreasing the value of surface boundary layer moisture required for the convection to occur over the western equatorial Pacific

More Related