 Welcome back. In our last video, we saw accumulated soil temperatures in no-till catching up with conventional till around the beginning of July. Let's get back to the conventional vs no-till data to see how that happened. If we have a look, not at accumulated heat units but actual temperatures, we've got maximum and minimum temperatures. These are the maximum for the no-till vs conventional and then the minimum temperatures. Again, going back to what you were saying, we had a lower maxima here but the actual maxima actually went higher in the middle part of June for the no-till soils. What was happening then? I think what we're seeing is that advanced growth in the conventional till corn there and it's probably canopying that roll a little bit quicker and shading it and we see those temperatures go down. So the no-till is yet to fully become canopied and it's able to take in more heat and store more heat and that's that part of catching up that it does. I got you. There was one last thing that I observed towards the end is our maximums in the no-till system looked a little bit lower and our minima looked a little bit higher. So would you care to comment on that? Well, I think we have that buffering effect that Anthony talked about at the beginning and which is really good for soil biology. They don't like those big swings in temperature so we're going to not get as hot but we're not going to get as cold at night either. Keep a more constant, more steady temperature. That's so cool. So not only does residue act as soil armor for rain and wind, it acts as a blanket creating this elegant microclimate below ground. So what's next? How about we take a look at what most influences soil temperatures over the whole growing season. See you soon.