In the published paper [1], the plot sizes of Figure 4, Figure 6 and Figure 9 were incorrect. The correct Figures are as follows:
Figure 4.
Scatter plot of the GOSAT TANSO-FTS XH2O and coincident TCCON soundings (criteria of ±30 min and ±1° in latitude/longitude). For these criteria, there are no coincident TANSO-FTS ocean scans. The caption and color-coding are identical to those of Figure 3.
Figure 6.
Scatter plot of the GOSAT TANSO-FTS XH2O and coincident TCCON soundings (criteria of ±30 min and ±1° in latitude/longitude) at the Lamont (left) and Lauder (right) TCCON sites. All coincidences were found for TANSO-FTS land scans.
Figure 9.
Relative differences (GOSAT-TCCON)/TCCON as a function of the difference, in meters, between the retrieved altitude of the GOSAT footprints and the altitude of the TCCON sites, for GOSAT land scans only. The caption and color-coding are identical to those of Figure 3.
We apologize for any inconvenience caused to the readers by these changes. The manuscript will be updated and the original will remain available on the article webpage.
References
- Dupuy, E.; Morino, I.; Deutscher, N.M.; Yoshida, Y.; Uchino, O.; Connor, B.J.; De Mazière, M.; Griffith, D.W.T.; Hase, F.; Heikkinen, P.; et al. Comparison of XH2O Retrieved from GOSAT Short-Wavelength Infrared Spectra with Observations from the TCCON Network. Remote Sens. 2016, 8, 414. [Google Scholar] [CrossRef]
© 2016 by the author; licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC-BY) license (http://creativecommons.org/licenses/by/4.0/).