Zobrazeno 1 - 10
of 57
pro vyhledávání: '"D S Turner"'
Autor:
Z. Mariani, K. Strong, M. Wolff, P. Rowe, V. Walden, P. F. Fogal, T. Duck, G. Lesins, D. S. Turner, C. Cox, E. Eloranta, J. R. Drummond, C. Roy, D. D. Turner, D. Hudak, I. A. Lindenmaier
Publikováno v:
Atmospheric Measurement Techniques, Vol 5, Iss 2, Pp 329-344 (2012)
The Extended-range Atmospheric Emitted Radiance Interferometer (E-AERI) is a moderate resolution (1 cm−1) Fourier transform infrared spectrometer for measuring the absolute downwelling infrared spectral radiance from the atmosphere between 400 and
Externí odkaz:
https://doaj.org/article/a599885172eb475a9d99ae60c626bab5
Autor:
Glen Lesins, Edwin W. Eloranta, Zen Mariani, I. A. Lindenmaier, James R. Drummond, P. F. Fogal, M. A. Wolff, Von P. Walden, David Hudak, D. S. Turner, C. Roy, Christopher J. Cox, Penny M. Rowe, Thomas J. Duck, David D. Turner, Kimberly Strong
Publikováno v:
Atmospheric Measurement Techniques, Vol 5, Iss 2, Pp 329-344 (2012)
The Extended-range Atmospheric Emitted Radiance Interferometer (E-AERI) is a moderate resolution (1 cm−1) Fourier transform infrared spectrometer for measuring the absolute downwelling infrared spectral radiance from the atmosphere between 400 and
Autor:
Y. J. Rochon, D. S. Turner
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 138:483-499
A fast forward radiative transfer model to compute the emitted limb radiances for use in recovering line-of-sight Doppler winds from thermal line emission has been developed and evaluated. This study was formulated around the Stratospheric Wind Inter
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 133:1547-1558
Radiances measured by remote-sensing instruments are now the largest component of the atmospheric observation network. The assimilation of radiances from nadir sounders involves fast radiative transfer (RT) models which project profiles provided by f
Publikováno v:
Journal of Applied Meteorology. 38:541-554
A continuous assimilation of high-density global satellite observations is required in order to improve numerical weather prediction analyses used to start forecasts. Until now, it was assumed that efficiency requirements imposed the use of regressio
Publikováno v:
Nutrient Cycling in Agroecosystems. 55:175-185
Fifteen field trials were conducted to evaluate soil mineral N measurement as a means for quantifying the total N supply to forage maize and so to form the basis for fertilizer recommendations on a crop-specific basis. In every trial, 4 rates of catt
Publikováno v:
Journal of Geophysical Research: Atmospheres. 103:11505-11528
A matrix parameterization of the 15 μm CO2 band radiative cooling in the middle and upper terrestrial atmosphere for both local thermodynamic equilibrium (LTE) and non-LTE (NLTE) layers is proposed. For the atmospheric region between ∼13 and 85 km
Autor:
J W Hall, D S Turner
Publikováno v:
Transportation Research Record: Journal of the Transportation Research Board. 1612:26-33
The conception, development, and adoption of early AASHO highway design criteria are documented. Examining the early efforts states used to select a design vehicle and develop horizontal curve design criteria illustrates why AASHO’s leadership was
Publikováno v:
The Journal of Agricultural Science. 127:441-449
SUMMARYA field experiment was conducted at nine sites in England (1991–94) to compare six sown species of cover crop and natural regeneration in terms of nitrogen uptake and effect on response to applied N by a subsequent spring barley crop. The su
Autor:
Thomas J. Duck, M. A. Wolff, C. Roy, James R. Drummond, Glen Lesins, P. F. Fogal, Von P. Walden, I. A. Lindenmaier, D. S. Turner, Kimberly Strong, Christopher J. Cox, Edwin W. Eloranta, Zen Mariani, David Hudak, Penny M. Rowe, David D. Turner, R. L. Lachance
Publikováno v:
SPIE Proceedings.
The Extended-range Atmospheric Emitted Radiance Interferometer (E-AERI) is a moderate resolution (1 cm−1) Fourier transform infrared spectrometer for measuring the absolute downwelling infrared spectral radiance from the atmosphere between 400 and