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@@ -6,7 +6,7 @@ This is the code described in Al-Attabi et al. (2021) for the inversion of the 2
 Although the wind wave inversion part is identical to that described in Alattabi et al., (2019), the swell inversion part is different. It is based on the Lipa and Barrick (1980) method (referred to as LPMP in the paper). Prior to the inversion, the 2nd order Doppler spectrum is separated into the swell and wind wave regions. For each region the inversion takes place separately and then the two (swell and wind wave) inverted spectra are combined to a single wave energy spectrum. The code includes the basic functions and a demo routine that uses the data of event A to H (see Al-Attabi et al, 2021) and recreates Figures 14 and 15 in the paper.  These figures might be slightly different (improved) because of a small change in the method used combining the swell and wind inverted spectra when no swell is detected. See comments inside the code for more details.
 
 - Code Citation:  
-Zaid Alattabi, Douglas Cahl & George Voulgaris, (2021, July 23). Swell Wave Radar Inversion Code (SWaveRIC) V1.0.1 (Version V1.0.1). Zenodo. http://doi.org/cc.cccc/zenodo.xxxxxxx
+Zaid Al-Attabi, Douglas Cahl & George Voulgaris, (2021, July 23). Swell Wave Radar Inversion Code (SWaveRIC) V1.0 (Version V1.0). Zenodo. http://doi.org/cc.cccc/zenodo.xxxxxxx
 
 - Method Citation:  
 Al-Attabi, Z.R., G. Voulgaris, and D.C. Conley, 2021. Evaluation and Validation of HF Radar Swell and Wind Wave Inversion Method. J. Atmos. Oceanic Technol., https://doi.org/10.1175/JTECH-D-20-0186.1