- About
- The Science
- CLIVAR Frontiers and Imperatives
- Frontier 1: Anthropogenic Climate Change
- Frontier 2: Decadal variability, predictability and prediction
- Frontier 3: Intra-seasonal and seasonal predictability and prediction
- Imperative 1: Improved atmosphere and ocean component models of Earth System Models
- Imperative 2: Data synthesis, analysis, reanalysis and uncertainty
- Imperative 3: Ocean observing system
- Imperative 4: Capacity building
- CLIVAR Endorsed Projects & Activities
- CLIVAR Objectives
- CLIVAR Successes
- CLIVAR Frontiers and Imperatives
- Panels and Working Groups
- Global
- PAGES/CLIVAR Intersection Working Group
- CCl/CLIVAR/JCOMM Expert Team on Climate Change Detection and Indices (ETCCDI)
- Global Synthesis and Observations Panel (GSOP)
- WGCM/CLIVAR Working Group on Ocean Model Development (WGOMD)
- Working Group on Seasonal to Interannual Prediction
- Working Group on Coupled Modelling (WGCM)
- Regional
- National Programmes
- Global
- Extremes Cross-Cut
- Calendar
- Resources
- Publications
About Us
Modes of Climate Variability in the Atlantic Sector. The figure on the right shows the path and strength of winter storms depending on the sign of the NAO; the location of tropical rainfal (determined by the ITCZ); and the transport of the ocean currents (MOC). Blue arrows:cold, deep currents; red arrows:warm surface currents (source: M. Visbeck, 2002; Science 297, 2223-2224)
