Total ozone dependence of the difference between the empirically corrected EP-TOMS and high-latitude station datasets

2009 ◽  
Vol 30 (15-16) ◽  
pp. 4283-4294 ◽  
Author(s):  
V. Kravchenko ◽  
A. Evtushevsky ◽  
A. Grytsai ◽  
G. Milinevsky ◽  
J. Shanklin
2006 ◽  
Vol 38 (11) ◽  
pp. 2374-2379 ◽  
Author(s):  
J.-K. Chung ◽  
Y.H. Kim ◽  
Y.-I. Won ◽  
B.K. Moon ◽  
T.H. Oh

2021 ◽  
Vol 67 (3) ◽  
pp. 230-235
Author(s):  
I. V. Polyakov

Changes of high-latitude freshwater content (FWC) play an important role in shaping the variability of polar oceans. FWC is defined as depth-integrated departure of salinity from a reference salinity Sref divided by this Sref . A constant Sref is often used for high-latitude FWC estimates. Here it is argued that for analyzing FWC spatiotemporal changes the use of local mean Sref is a better choice. Analysis of 2007 FWC anomalies in the 25–75 m layer demonstrated, for example, that the choice of Sref = 34.8 (which is often used in climate studies) leads to FWC spatial anomalies exaggerated, on average, by ~0.6 m, which is a substantial fraction of total spatial FWC changes. The problem is aggravated in areas where the difference between the local Sref and Sref = 34.8 is greater. Thus, it is concluded that using climatological mean salinities as Sref provides superior estimates of spatiotemporal Arctic Ocean FWC changes.


1997 ◽  
Vol 102 (D7) ◽  
pp. 9029-9038 ◽  
Author(s):  
C. G. Wellemeyer ◽  
S. L. Taylor ◽  
C. J. Seftor ◽  
R. D. McPeters ◽  
P. K. Bhartia

2014 ◽  
Vol 2 (5) ◽  
pp. 82-86
Author(s):  
Prakash Khatarkar ◽  
◽  
Varsha Kachneria ◽  
Harleen Kaur ◽  
Roshni Atulkar ◽  
...  

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