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An Experimental Approach to the Evaluation of Prescribed Fire Behavior
Mueller, Eric V., Clark, Kenneth L., Kremens, Robert L., Gallagher, Michael R., Thomas, Jan C., Houssami, Mohamad El., Filkov, Alexander I., Butler, Bret W., Hom, John, Mell, William E., Simeoni, Albert, Skowronski, Nicholas S.
The wind regime of the mesosphere and lower thermosphere during the DYANA campaign-I. Prevailing winds
Singer W., Hoffmann P., Manson A., Meek C., Schminder R., Kürschner D., Kokin G., Knyazev A., Portnyagin Y., Makarov N., Fakhrutdinova A., Sidorov V., Cevolani G., Muller H., Kazimirovsky E., Gaidukov V., Clark R., Chebotarev R., Karadjaev Y.
were located between 107°W and 102°E, mostly in northern mid-latitudes with well covered areas
The wind regime of the mesosphere and lower thermosphere during the DYANA campaign-II. Semi-diurnal tide
Portnyagin Y., Makarov N., Chebotarev R., Nikonov A., Kazimirovsky E., Kokourov V., Sidorov V., Fakhrutdinova A., Cevolani G., Clark R., Kürschner D., Schminder R., Manson A., Meek C., Müller H., Stoddart J., Singer W., Hoffmann P.
An ultra-spatially resolved method to quali-quantitative monitor particulate matter in urban environment
Baldacchini C., Sgrigna G., Clarke W., Tallis M., Calfapietra C.
Variability of the quasi-2-day wave observed in the MLT region during the PSMOS campaign of June-August 1999
Pancheva D., Mitchell N., Manson A., Meek C., Jacobi C., Portnyagin Y., Merzlyakov E., Hocking W., MacDougall J., Singer W., Igarashi K., Clark R., Riggin D., Franke S., Kürschner D., Fahrutdinova A., Stepanov A., Kashcheyev B., Oleynikov A., Muller H.
ranging from 21°N to 75°N and longitudes from 142°E to 157°W. The data were examined to investigate
Mesosphere/lower thermosphere prevailing wind model
Portnyagin Y., Solovjova T., Merzlyakov E., Forbes J., Palo S., Ortland D., Hocking W., MacDougall J., Thayaparan T., Manson A., Meek C., Hoffmann P., Singer W., Mitchell N., Pancheva D., Igarashi K., Murayama Y., Jacobi C., Kuerschner D., Fahrutdinova A., Korotyshkin D., Clark R., Taylor M., Franke S., Fritts D., Tsuda T., Nakamura T., Gurubaran S., Rajaram R., Vincent R., Kovalam S., Batista P., Poole G., Malinga S., Fraser G., Murphy D., Riggin D., Aso T., Tsutsumi M.
Global-scale tidal variability during the PSMOS campaign of June-August 1999: Interaction with planetary waves
Pancheva D., Merzlyakov E., Mitchell N., Portnyagin Y., Manson A., Jacobi C., Meek C., Luo Y., Clark R., Hocking W., MacDougall J., Muller H., Kürschner D., Jones G., Vincent R., Reid I., Singer W., Igarashi K., Fraser G., Fahrutdinova A., Stepanov A., Poole L., Malinga S., Kashcheyev B., Oleynikov A.
The wind regime of the mesosphere and lower thermosphere during the DYANA campaign-I. Prevailing winds
Singer W., Hoffmann P., Manson A., Meek C., Schminder R., Kürschner D., Kokin G., Knyazev A., Portnyagin Y., Makarov N., Fakhrutdinova A., Sidorov V., Cevolani G., Muller H., Kazimirovsky E., Gaidukov V., Clark R., Chebotarev R., Karadjaev Y.
were located between 107°W and 102°E, mostly in northern mid-latitudes with well covered areas
Utilization of remote sensing techniques for the quantification of fire behavior in two pine stands
Skowronski, Nicholas S., Clark, Kenneth L., Gallagher, Michael R., Kremens, Robert L., Thomas, Jan C., Houssami, Mohamad El, Filkov, Alexander I., Hadden, Rory M., Mell, William E., Mueller, Eric V., Simeoni, Albert
, with spread occurring predominantly in the surface fuels with intensities in the range of 200–4400 kW m-1
The wind regime of the mesosphere and lower thermosphere during the DYANA campaign-II. Semi-diurnal tide
Portnyagin Y., Makarov N., Chebotarev R., Nikonov A., Kazimirovsky E., Kokourov V., Sidorov V., Fakhrutdinova A., Cevolani G., Clark R., Kürschner D., Schminder R., Manson A., Meek C., Müller H., Stoddart J., Singer W., Hoffmann P.

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