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WEIGHTED LOCAL MORREY SPACES
Nakamura S., Sawano Y., Tanaka H.
Superconductivity of Pb ultrathin film on Ge(111) surface
Toyama, H., Huang, H., Nakamura, Toshio., Bondarenko, Leonid V., Tupchaya, Aleksandra Y., Gruznev, Dmitriy V., Takayama, A., Zotov, Andrey V., Saranin, Aleksandr A., Hasegawa, S.
Conditions for boundedness into Hardy spaces
Grafakos L., Nakamura S., Sawano Y., Van Nguyen H.
Renal allograft arteriovenous fistula and large pseudoaneurysm
Nakatani Tatsuya, Uchida Junji, Han Y.S., Iwai Tomoaki, Nakamura Kenji, Kawashima Hidenori, Sugimura Kazunobu
Magnon BEC in antiferromagnets with Suhl-Nakamura interaction
Tagirov M., Alakshin E., Bunkov Y., Gazizulin R., Gazizulina A., Isaenko L., Klochkov A., Safin T., Safiullin K., Zhurkov S.
Magnon BEC in antiferromagnets with Suhl-Nakamura interaction
Magnon BEC in antiferromagnets with Suhl-Nakamura interaction
Tagirov M., Alakshin E., Bunkov Y., Gazizulin R., Gazizulina A., Isaenko L., Klochkov A., Safin T., Safiullin K., Zhurkov S.
Magnon BEC in antiferromagnets with Suhl-Nakamura interaction
HRDI observations of mean meridional winds at solstice
Lieberman R., Robinson W., Franke S., Vincent R., Isler J., Fritts D., Manson A., Meek C., Fraser G., Fahrutdinova A., Hocking W., Thayaparan T., MacDougall J., Igarashi K., Nakamura T., Tsuda T.
of the globe. Peak equatorward winds of about 15 m s-1 are usually observed in the summer hemisphere near 30
Comparison of mesospheric and lower thermospheric residual wind with High Resolution Doppler Imager, medium frequency, and meteor radar winds
Lieberman R., Smith A., Franke S., Vincent R., Isler J., Manson A., Meek C., Fraser G., Fahrutdinova A., Thayaparan T., Hocking W., MacDougall J., Nakamura T., Tsuda T.
from the summer toward the winter hemisphere. Peak values exceed 20 m s-1 and are observed
HRDI observations of mean meridional winds at solstice
Lieberman R., Robinson W., Franke S., Vincent R., Isler J., Fritts D., Manson A., Meek C., Fraser G., Fahrutdinova A., Hocking W., Thayaparan T., MacDougall J., Igarashi K., Nakamura T., Tsuda T.
of the globe. Peak equatorward winds of about 15 m s-1 are usually observed in the summer hemisphere near 30
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.

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