I had luck with the wind again today. I was glad because it was stronger than it was yesterday. Or, perhaps, it just seemed that way because most of today's ride took me along shorelines. Also, the sky was even clearer than it was yesterday, and large bodies of water magnify the sun's rays. Sometimes I think long exposure to direct sunlight tires me out even more than the wind, or anything else.
Anyway, I rode to Point Lookout today. It's not as long as the ride to Connecticut, and it's almost entirely flat. There is one fairly long gradual incline up Woodhaven Boulevard from Jamaica Avenue to Forest Park. Even though it's near the end of my ride, it isn't very arduous.
Best of all, the wind was at my back, as it was from the time I turned on to the Veterans Memorial Bridge from Rockaway Beach. That meant, of course, that I pedaled into the wind on my way out, and that it blew from the Atlantic onto my right side on my way to the Point, and onto my left on my way back.
The thing that struck me most about today's ride, though, was at Point Lookout. The tide was out--and I mean really out. There were no boats in the water. Most telling, though, was this:
A family picnic on the sandbar! I've never seen it so long or wide. It was like a boardwalk, with all of the people walking their dogs and toddlers toddling on it. Naturally, no one was fishing.
Now, I am no climate scientist. In fact, I can't claim to be a scientist of any sort. So perhaps I am revealing my ignorance in describing the observation you are about to read and the question I will pose from it.
As I understand it, the extreme blizzards so many places experienced during the past few winters are actually a result of global warming: Increasing temperatures, especially in the oceans, are causing the atmospheric instability that leads to all kinds of storms, including blizzards and ice storms as well as hurricanes and tornadoes.
So I wonder whether tides that are receding further out (I've noticed this in other places besides Point Lookout) are a result of the rising sea level. Just as the tides are higher and stronger, could the pull-back also be stronger--enough to pull the tides further from the shoreline when they recede?
Again, I emphasize that I am not a scientist: What I am saying and asking is based entirely on observation and logic. Also, I know it doesn't directly relate to cycling. But what I see in the oceans, on the shorelines, in the hills or anyplace else is part of my rides. I can't help but to wonder what I will and won't see on future rides!
Anyway, I rode to Point Lookout today. It's not as long as the ride to Connecticut, and it's almost entirely flat. There is one fairly long gradual incline up Woodhaven Boulevard from Jamaica Avenue to Forest Park. Even though it's near the end of my ride, it isn't very arduous.
Best of all, the wind was at my back, as it was from the time I turned on to the Veterans Memorial Bridge from Rockaway Beach. That meant, of course, that I pedaled into the wind on my way out, and that it blew from the Atlantic onto my right side on my way to the Point, and onto my left on my way back.
The thing that struck me most about today's ride, though, was at Point Lookout. The tide was out--and I mean really out. There were no boats in the water. Most telling, though, was this:
A family picnic on the sandbar! I've never seen it so long or wide. It was like a boardwalk, with all of the people walking their dogs and toddlers toddling on it. Naturally, no one was fishing.
Now, I am no climate scientist. In fact, I can't claim to be a scientist of any sort. So perhaps I am revealing my ignorance in describing the observation you are about to read and the question I will pose from it.
As I understand it, the extreme blizzards so many places experienced during the past few winters are actually a result of global warming: Increasing temperatures, especially in the oceans, are causing the atmospheric instability that leads to all kinds of storms, including blizzards and ice storms as well as hurricanes and tornadoes.
So I wonder whether tides that are receding further out (I've noticed this in other places besides Point Lookout) are a result of the rising sea level. Just as the tides are higher and stronger, could the pull-back also be stronger--enough to pull the tides further from the shoreline when they recede?
Again, I emphasize that I am not a scientist: What I am saying and asking is based entirely on observation and logic. Also, I know it doesn't directly relate to cycling. But what I see in the oceans, on the shorelines, in the hills or anyplace else is part of my rides. I can't help but to wonder what I will and won't see on future rides!
