... These 2 to 3 year variations may be com pletely explained by the geophysical excitation 494 38 Baltic GORSHKOV m stations 40 20 Western Europe, 8 stations 0 Japan, 8 stations 20 Eastern coast of the United States, 24 stations 40 1860 1880 1900 1920 1940 ...
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Ссылки http://www.gao.spb.ru/english/as/publ/gorshkov_ssr-2010.pdf -- 433.4 Кб -- 08.08.2011 Похожие документы
... In the range of 2 to 600 M the spectrum has a spectral index of 0.8 0.1, in the range of 0.6 to 2 M the spectral index is 3.0 1, and in the range of 600 to 2104 M the spectral index is 0.7 0.3. ...
... phase NLSM fit Period, years ~100-year omponent 117.8 ~50-year component 1-order trend 50.9 Amplitude 59 dg 34 dg 2dg /year Phase (1880) -118o 95 o Excitation forecast L.V.Zotov, C. M. Bizouard Chandler wobble and its excitation depending on the filter ...
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Ссылки http://www.gao.spb.ru/english/as/j2014/presentations/zotov.pdf -- 2221.7 Кб -- 28.09.2014 Похожие документы
... reduce now to a a 2 + k a2 = 8 G 3 ( ff + ) , a Ё a = 8 G 3 (f f - ) ; here k equals ... Two other equations result in 8 G 3 ( ff (1) + ) = f 2, 8 G 3 1Ё =- f. 2 ... Rewrite previous equations as a=- 8 G 3 a + , a= Ё 8 G 3 a (f f - ). ff At first ...
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Ссылки http://www.gao.spb.ru/russian/psas/ffk2013/tfiles/Khriplovich_NBB1slides.pdf -- 87.7 Кб -- 25.11.2013 Похожие документы
... Monday . 7 Oct . Tuesday . 8 Oct . Wednesday . 9 Oct . Thursday . ... 1. Korzinin E. 2. Ivanov V. 3. Gorshteyn M. 1. Onegin M. 2. Altaisky M. 3. ... Ivanov V. 3. Gorshteyn M. 1. Onegin M. 2. Altaisky M. 3. Pitjeva E. (year) . 4. ...
... Septem ber 2014 6 M ODULATION MEASUREMENT OF THE GRAVITATIONAL FREQUENCY SHIFT 1103 km 210-10 3105 km 710-10 H-maser Frequency stability at ~1 day, Df / f 410-15 Cs-fountain ~110-16 e-parameter error, de (after 100 orbits) 110-6 310-8 Journees 2014, Saint ...
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Ссылки http://www.gao.spb.ru/english/as/j2014/presentations/litvinov.pdf -- 2369.8 Кб -- 28.09.2014 Похожие документы
... primordial per turbations The same potential, the same at the end of inflation e.g. F.Bezrukov, D.G., M.Shaposhnikov (2008) V 2 M 0.20 2 P n s 1- 8(4N + 9) , (4N + 3)2 r 192 (4N + 3)2 0.15 But WMAP observes different N in the two models: k /a0 = 0.002/Mpc ...
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Ссылки http://www.gao.spb.ru/russian/psas/ffk2013/tfiles/Gorbunov_FFK-2013.pdf -- 1790.8 Кб -- 25.11.2013 Похожие документы