the salinity and the surface temperature. you might get a difference in temperature between a lower layer and an upper layer and a difference in salinity, in density. and this would affect the path of sound waves. and so the two ping signals could very well be coming from a signal source. and with all the errors adding up, they seem to be very far apart. but if you re going to look some place, this is sure a very good start. yeah. jeff, we are learning tonight that the pings detected by the ocean shield, as bill nye was just referencing, were actually at 33.3, where he said you may get a different temperature, right? a lower standard than the standard beacon frequency of 37.5 kilohertz. that s according to the pinger manufacturer. do you think this could still be the black boxes in your estimation, even at these different temperatures or different rates? there s a lot of problems with this pinger data. the 33.3 megahertz frequency, that s a big problem.
there s been storms in this part of the ocean, which will change the salinity and the surface temperature. you might get a difference in temperature between a lower layer and an upper layer and a difference in salinity, in density. and this would affect the path of sound waves. and so the two ping signals could very well be coming from a signal source. and with all the errors adding up, they seem to be very far apart. but if you re going to look some place, this is sure a very good start. yeah. jeff, we are learning tonight that the pings detected by the ocean shield, as bill nye was just referencing, were actually at 33.3, where he said you may get a different temperature, right? a lower standard than the standard beacon frequency of 37.5 kilohertz. that s according to the pinger manufacturer. do you think this could still be the black boxes in your estimation, even at these different temperatures or different rates? there s a lot of problems with this pinger data.