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Status Replies posted by mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Thanks for the catch on the elliptical orbit. Also another issue is Moons. These equations modify a lot for them if I am not mistaken I will have to spend some time thinking about them.
Now for some good news. There is a much easier way to find the prime meridian. If you know all the planet and moons orientation of the 0o 0' 0" longitude mark relative to the fixed KSP X axis at t=0 and you know where the X axis is relative to each planet then you can solve for the rest. It just so happens that this information is in a file somewhere in the KSP INI for the planets. The mean anomaly is PI for Kerbin and the initial rotation for Kerbin's initial rotation is 90 degrees relative to this axis (from hyperedit) so that means the x axis points directly from the center of kerbin to cent of the sun. Problem solved. well at least that part is solved now to actually do the math. At least I don't have to spend hours doing this experimentally. Threre where a lot of people that helped me figure this out so the only credit i get is asking enough questions.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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OK So getting the exact initial orientation of each of the planets and moons could be a challenge. NathanKell was so kind as to give us the exact orientation of Kerbin but the others could be problematic. I do have enough info to predict the temperature at any location on Kerbin at any time of day or night at any altitude but the other planets are hopelessly out of reach, without accurate initial orientation parameters.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Quote
For one thing you're not dealing with a perfect sphere, you're dealing with a fairly low-resolution polygonal approximation. That has something to do with it, surely?
Sure it does. So should I consider the solar panels catching light through the water(wor whatever passis for water on Eve) several minutes before sunrise a bug or working as intended or somewhere in between?
Also not sure how I can account for this except to finish working out my Kerbin temp calculator and test and see if I need to adjust it or not.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Quote
By the way, in real life, sunrise is defined at the time when the Sun's upper limb touches the horizon. By this definition, sunrise in KSP should occur 66 seconds earlier than the rise of the solar center.
To be sure that makes sense, I think you may be onto something. I wonder if no one noticed because no one wanted an accurate local clock in KSP before. I am guessing no really needed to measure exactly when sunrise happens before. In any case it does not matter as long as the same definition of sunrise is used for all measurements. Since KSP solar panel gives a nearly instantaneous feedback I am going to hope that is correct and go with that trigger unless something else tells me otherwise. The question then becomes will our calculations be off enough to matter if we use this definition since the proper definition of sunrise will determine whether or not our calculations for temp matches the numbers ksp puts out of a given place and time.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
-
Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
-
Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
-
Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Quote
Temperature = atmosphereTemperatureCurve + atmosphereTemperatureOffset * atmosphereTemperatureSunMultCurve
where,
atmosphereTemperatureOffset = latitudeTemperatureBiasCurve + latitudeTemperatureSunMultCurve * sunDotNormalized
just to confirm if I rewrite this as expanded Temperature = atmosphereTemperatureCurve+ ((latitudeTemperatureBiasCurve + (latitudeTemperatureSunMultCurve * sunDotNormalized))*atmosphereTemperatureSunMultCurve)
Expanding this gives Temperature = atmosphereTemperatureCurve+ (latitudeTemperatureBiasCurve*atmosphereTemperatureSunMultCurve) + (latitudeTemperatureSunMultCurve *atmosphereTemperatureSunMultCurve* sunDotNormalized)
Also I am having a heck of a time remembering my spherical coordinate trigonometry any chance you could feed me the formulas for getting the minimum SZA and Maximum SZA for a given latitude.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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I Spent the morning using hyperedit and got 2:59:43 at 0o 0' 0" this is when the solar panels activated. Also did Duna but I will have to redo since 0o 0' 0" is at 2600m elevation on duna. I will install scansat and find a sea level coordinate along the equatorial plane and use that as the Greenwich meridian for duna I also did Eve but I ended up reporting a bug after the Eve attempt due to oceans having 100% transparency thus reporting sunrise far earlier than it really happens. The bug report is here I probably did not do this correctly. I think I can work around that bug.
Also it had occurred to me this morning that is was the KSC altitude that gave most of the error, but it looks like you figured it out befor I got around to telling you. I wonder what accounts for the remaining 15-17 seconds.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hmm... well... then I think I am going to determine sunrise at KSC with solar panels and calculate from there just to be sure. though the 94 meter offset might be a problem. Hmm maybe I should find an ocean view. I do want it to be exact. It is going to be additionally challenging doing the other planets.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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I just so happen to know approximately when noon is at KSC it occurs for the first time 0d 0h 15m 0s but only approximately based on observation that would put the first sun rise at approximately at 0d 4h 30m 0s @NathanKell perhaps you could shed some light on this. it is not like a can take a sextant into the game to measure this exactly though solar panels may provide a solution since they trigger nearly instantaneously. I will want to at least know to the nearest second. Otherwize it could be calculation breaking.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Yes I can confirm this to be true... oh doh I was over complicating it... but wait you still need to know when sunrise will occur at your location which means you still need to know the greenwich equivalent... and what about the other planets they will still need their own greenwich equivalent, unless the game broadcasts the solar hour angle for all the planets.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Nope did not take me long to realize there is an additional snag in all this even before I crunch some more numbers. Time! You don't need to just know where you are on a planet you need to know where you are relative to Kerbin time 0d 0h 0m 0s and relative to a longitudinal point on the planet whose position relative to the sun at that time is known. This must be known for every planet with atmo. (Sol is fully static with no rotation at all?) Also unless the rotational period is exactly a multiple of orbital period there will be no simplifying this other than to calculate the least common factor of the two. (maybe all of this has already been done, part of me says yes but I do not know where to find it.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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@Overengineer1 you are sooo far ahead of me on this. But I think I begin to see the challenge and why the whole trajectory would need to be simulated and the optimal solution found. The number of variables that come into play start to be a bit overwhelming. Which makes your work all the more amazing. I am going to say that this has been very enlightening to me. Thank you for your patience.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3
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Quote
Since temperature varies on a 6-hour cycle, the atmosphere also fluctuates on the same 6-hour cycle
Yes, relative to the surface of Kerbin this is true. But relative to the Sol it never varies. It is as if the Atmosphere is tidally locked with the sun. Your explanation above would seem to confirm this.
In any case wow you must have spent hours working all of this out. Bravo. Excellent and very understandable. Thank you Thank you, Thank You. I wish I could repay you. You should really share all of this with the community as a whole, I can't be the only one who could benefit from the new understanding.
QuoteThere's a way but I don't know how to do it. NathanKell knows how, so you might try asking him.
Will do.
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Hi OhioBob.
Nathankell suggested I contact you about the nature of the atmosphere in KSP...so here I am. I am at this time working on the static pressures (will tackle static temp after and am collecting data for both) on Kerbin using graphotron 2000. I really don't know much since I have only run numbers on one csv data output (though I have several more wait for analysis) at this point but I will give you my best guess on how I expect static pressure on kerbin to work.
I am guessing that all though the planet rotates every 6 hours the Atmosphere behaves as if it only rotates once a year. (which is to say there should be a174 mph wind at the equator but ... there is no wind in ksp) In other words the temp and pressure above the point 0o 0' 0" latitude and 0o 0' 0" longitude at noon each kerbin day has the highest Temp and lowest pressure at the surface of any point on kerbin at that time. I am further guessing that the pressure with altitude follows the following formula Atmospheric Pressure= Caltitude*e-(A)*Altitude(m)
Pressure versus change in longitude with a fixed time and fixed altitude would follow; pressure=Clogitude*cos(beta)and pressure versus change in latitude with a fixed time and fixed altitude would be; pressure=Clatitude*sin(theta/2)
(this should all be in spherical coordinates)
Am I even in the right ball park? Please feel free to correct me or to tell me I am crazy. I really am looking to derive, from experimental data if necessary a three dimensional formula that will yield the static air pressure (and temperature eventually) for any place and time on kerbin and eventually the other planets with atmospheres as well.
I of course don't have a strong need to do all the work myself, no need to reinvent the wheel if the work is already done, so if you have already figured all this out please feel free to share.
Much of my calculus is very rusty so please go easy on me.
Looking forward to your thoughts.and Thank You,
mcirish3