All of these elements are
variable on decadal scales — including ocean heat.
Not exact matches
That is precisely what I have done: Using annual sunspot number as a representative of the long term (
on the
decadal scale) solar magnetic field impact and small
variable component of the Earth's magnetic field, as calculated from data by Jackson and Bloxam.
The slower components of the climate system (e.g. the ocean and biosphere) affect the statistics of climate
variables (e.g. precipitation) and since they may feel the influence of their initial state at multi
decadal time
scales, it is possible that climate changes also depend
on the initial state of the climate system (e.g. Collins, 2002; Pielke, 1998).
Ice, cloud and terrestrial water storage are
variable on decadal to millennial
scales at least.
Environmental
variables estimated over larger spatial and temporal
scales included the upwelling index (UI) for 48 ° N, 125 ° W (http://www.pfeg.noaa.gov), an indicator of upwelling strength based
on wind stress measurements, as well as the Pacific
Decadal Oscillation (PDO, http://jisao.washington.edu/pdo/PDO.latest), a composite indicator of ocean temperature anomalies [33], seawater temperature from Buoy 46041 ∼ 50 km to the southwest from Tatoosh (www.ndbc.noaa.gov), and remote sensing of chl a (SeaWiFS, AquaModis).