Table 2.
A review of parameterizations provided for the relationship between Nd and Na
Region | a | β | r | Highest Na(cm−3) | Study |
---|---|---|---|---|---|
Northeast Pacific | 7.73 | 0.56 | 0.78 | 500 | This study (non-BB) |
Northeast Pacific | 33.25 | 0.26 | 0.70 | 1,800 | This study (BB) |
Around the British Isles and over the Atlantic near the Azores Islands | 14 | 0.26 | 0.95 | 12,000 | Raga and Jonas (1993) |
Houston and the northwestern Gulf Of Mexico | 33.3 | 0.26 | 0.66 | 11,000 | Lu et al. (2008) |
Vicinity of Houston, TX | 36.3 | 0.35 | N/A | 10,000 | Jiang et al. (2008) |
Southeast Pacific | 7.7 | 0.55 | 0.89 | 600 | Terai et al. (2012) |
Northeast Atlantic and North Pacific | 2.75 | 0.73 | N/A | 400 | O'Dowd et al. (1999)a |
Northeast Pacific | 1.03 | 0.96 | 0.95 | 500 | Twohy et al. (2005)b |
Pacific offshore of California, Chile, and Atlantic offshore of Namibia | 13.39 | 0.51 | 0.94 | 700 | Hegg et al. (2012)c |
Note. All mentioned parameterizations are from studies based on in situ measurements. Reported α and β values are either reported directly from a power law relationship or were derived from a different type of parameterization by power law fitting. Values reported in the r column belong to the original form of equations and N/A values denote that no correlation coefficient was provided by a particular study.
Originally presented in form of Nd = 197 (1 – exp(−6.13× 10−3 Na)).
Originally presented in form of Nd = −2.2 + 1.027 Na − 0.000837 Na2.
Originally presented in form of Nd = 0.72 Na + 47.