Skip to main content

Currently Skimming:

Frontiers and Research Opportunities
Pages 47-50

The Chapter Skim interface presents what we've algorithmically identified as the most significant single chunk of text within every page in the chapter.
Select key terms on the right to highlight them within pages of the chapter.


From page 47...
... , which would integrate the ocean and cryosphere response. Participants noted that adequate monitoring of climate change for studying decadal variability would truly require a combination of metrics, for example, the use of global sea level rise coupled with GMST.
From page 48...
...  Other specific areas that would benefit from improved observations include o geographical distribution of aerosols below 15 km to determine contribution of external forcing, and o ocean isotope geochemistry in the equatorial Pacific to determine El Niño/La Niña occurrences during the past 1,000 years. Modeling Challenges, Needs, and Opportunities Some individual participants identified additional modeling challenges, needs, and opportunities:  Regional patterns and cross-timescale interactions are important, but not all models can capture the full collection of processes and phenomena that have been deemed relevant to regional (or basin-scale)
From page 49...
... Other knowledge gaps include the following:  The connection between Arctic sea ice loss and mid-latitude weather, and the consequential regional effects;  The role of and quantitative data on stratification of the deep Southern Ocean;  The relative importance of atmospheric vs. oceanic bridges in linking stochastic processes at mid-to-high latitudes (how does local atmospheric forcing produce remote response(s)
From page 50...
... Some participants reiterated the importance of developing predictive capability for decadal variability of seasonal-to-interannual coupled ocean-atmosphere phenomena, including weather, for selected geographical areas for specific phenomena:  El Niño/La Niña  Tropical Atlantic  Arctic sea ice  Southern Ocean/Antarctic sea ice (surface winds, ocean stratification)  Bottom- and intermediate-water formation They noted, however, that some studies of predictability of this most recent, as well as other slowdown periods, have met with some success (see Toward Predictability)


This material may be derived from roughly machine-read images, and so is provided only to facilitate research.
More information on Chapter Skim is available.