MWR-064-03-0069The recently-developed Refsdal "aerogram" possesses the interesting property of providing an exceedingly simple, direct and exact means of evaluating geopotential, and hence altitude, from the graph of an aerological sounding. The aerogram includes, in fact, a geopotential scale on the right margin for this purpose
This report is a revision of the altitude pressure tables of the United States standard atmosphere g...
Knowledge of standard air temperature, pressure, density, speed of sound, and viscosity as a functio...
The theory of the rate-of-climb indicator is developed in a form adapted for application to the inst...
Though the method of adiabatic charts has been applied to thermodynamical problems in meteorology fo...
Geoaltitude coordinates of geometric height, pressure, temperature, density, and potential energy le...
During 1925 the assumption of an isothermal atmosphere which was in general use as the standard for ...
under research authorization formulated and recommended by the subcommittee on aero-dynamics and app...
The main task of this paper is to describe altitude measurement methods and specify how to process t...
This report is Section two of a series of reports on aeronautic instruments (Technical Report nos. 1...
Altimeter corrections for non-standard temperature pose a challenge because accurate calculations re...
This report was prepared at the request of the National Advisory Committee for Aeronautics and discu...
Explicit equations involving only square root and summation operations are derived for computing bar...
As an integral part of its program of geologic and ground-water studies, the Iowa Geological Survey ...
The hydrometeorologist is often confronted with the problem of determination of precipitable water i...
A comparison study was conducted to evaluate limitations of several atmospheric calibration techniqu...
This report is a revision of the altitude pressure tables of the United States standard atmosphere g...
Knowledge of standard air temperature, pressure, density, speed of sound, and viscosity as a functio...
The theory of the rate-of-climb indicator is developed in a form adapted for application to the inst...
Though the method of adiabatic charts has been applied to thermodynamical problems in meteorology fo...
Geoaltitude coordinates of geometric height, pressure, temperature, density, and potential energy le...
During 1925 the assumption of an isothermal atmosphere which was in general use as the standard for ...
under research authorization formulated and recommended by the subcommittee on aero-dynamics and app...
The main task of this paper is to describe altitude measurement methods and specify how to process t...
This report is Section two of a series of reports on aeronautic instruments (Technical Report nos. 1...
Altimeter corrections for non-standard temperature pose a challenge because accurate calculations re...
This report was prepared at the request of the National Advisory Committee for Aeronautics and discu...
Explicit equations involving only square root and summation operations are derived for computing bar...
As an integral part of its program of geologic and ground-water studies, the Iowa Geological Survey ...
The hydrometeorologist is often confronted with the problem of determination of precipitable water i...
A comparison study was conducted to evaluate limitations of several atmospheric calibration techniqu...
This report is a revision of the altitude pressure tables of the United States standard atmosphere g...
Knowledge of standard air temperature, pressure, density, speed of sound, and viscosity as a functio...
The theory of the rate-of-climb indicator is developed in a form adapted for application to the inst...