untitled
|
|
- さあしゃ ももき
- 5 years ago
- Views:
Transcription
1 1. [IPCC, 2001] ( ) [UNEP, 1997] [Yatagai and Yasunari, 1995] [Iwao and Takahashi, 2006] 4 [Morinaga and Shinoda, 2003] [Kurosaki and Mikami, 2003] Iwao and Takahashi [2006] [Enomoto et al., 2003; Nakamura and Fukamachi, 2004; Sato and Takahashi, 2006] Iwao and Takahashi [2006] Terao [1998] , (70N) 3,4 (1983 ) ( 1) (JJA) National Climatic Data Center (NCDC) Global Dail Climatolog Network (GDCN) Global Summar of Da (GSD) ECMWFERA low-ass filter Iwao and Takahashi [2006] 7 ( ) ( ) 39
2 1: 39 (JJA) ( ) EOF 1 (a)(b)(a) EOF EOF Iwao and Takahashi [2006] 3.2 ( q) 2 q = f0 + β + ψ + ρ0 ρ0εψ z = q z vor + q ( q )( q ) vor 2 2 ε = f 0 / N 3 (K) [Andrews et al., 1987; Hoskins and Ambrizzi, 1993; Nishii and Nakamura, 2004] 2 K q / u ε / 4H ( ) str a hPa Ertel (q)( ) ( ) 2 2b,c ( β ) = β u [Hoskins and Ambrizzi, 1993] [Ambrizzi et al., 1995; Enomoto et al., 2003] ( acos φ K ) 1 q str q vor str
3 2: (JJA) 300hPa (a) Ertel (0.1 PVU : 1 PVU=10-6 Km 2 kg -1 s -1 ) (b) q ( m -1 s -2 ) (c) vor q ( m -1 s -2 )(d) acos φ K (: 2, 4, 6, str 8, 10, 12, 15, 25-30; K 2 <0 ) 2c 10, hPa 40N 60N v (30-150E, 40 60N, 300hPa, JJA ) EOF 3 EOF 1 2 (VEOF1 VEOF2) 3: v (30-150E, 40 60N, 300hPa) (JJA) EOF (a) 1 (b) 2 VEOF1 VEOF2 VEOF1 VEOF2 40N 60N d 3 VEOF2 VEOF1 1/4 VEOF1 VEOF2 ()46 18 Terao [1998] (60N 70N) VEOF (VPC1 VPC2) VEOFs
4 4: (a) 7 (b) 7 VPC1 VPC2 (%) VPC1 4 ( 4a) ( 4b) VPC1 VPC2 EOF ( 1b) N E60N E VPC1 VPC2 ( 4 ) () 7 [Iwao and Takahashi, 2006] VMG VSB 5VMG 300hP wave activit flu [Takaa and Nakamura, 2001] VPC ( 5a-c) ( 5d) VSB () [e.g., Pell and Hoskins, 2003] () VMG -2 6 (90-120E)
5 6: VMG-2 (90-120E)(: m/s) (10-6 /s ; 0/s ) 5: 300hPa (VMG) 300hPa (20m ) wave activit flu () (a) -8(b) -4(c) 0 (d) 0 (0.25mm/da ) 95% (30-50N) (60-75N) Iwao and Takahashi [2006] ζ t = uζ vζ u ζ v ζ ζd ζ D NL F T = ut vt u T v T t ωθ ( NL Q 0 ) ω θ ( 0) NLFQ 1 6 F Q 1 NL 7 6ab 200hPa ( uζ ) ( ζd ) ( v ζ ) () uζ 5 uζ v ζ 1 c
6 4. 7: VMG-2 200hPa (a) uζ (b) ζ D (10-6 /sda ; ) 500hPa (c) ω θ ( 0) (d) Q 1 /c (K/da ; )850hPa (e) F (f) ζ D (10-6 /s da ; ) (e,f) 850hPa ( 7ef) ζd (F ) 500hPa ( 7cd) ω θ ( 0) Q 1 /c ( ) () (VMG) (VSB) VMG ( 4) VMG 180
7 (A-1, G-2, B-4) Ambrizzi T., B.J. Hoskins, and H.H. Hsu (1995), Rossb-wave roagation and teleconnection atterns in the austral winter, J. Atomos. Sci., 52, Andrews, D.G., J.R. Holton, and C.E. Leov (1987), Middle Atmoshere Dnamics, , Academic Press. IPCC (2001), Climate change 2001: The scientific basis, edited b Houghton J.T., Ding Y., Griggs D.J., Noguer M., Linden P.J.vd, Dai X., Maskell K., and Johnson C.A., Cambridge Universit Press. Iwao, K., and M. Takahashi (2006), Interannual change in summertime reciitation over northeast Asia, Geohs. Res. Lett., 33, L16703, doi: /2006gl Enomoto, T., B.J. Hoskins, and M. Matsuda (2003), The formation mechanism of the Bonin high in August. Quart. J. Ro. Meteor. Soc., 129, Hoskins B.J. and T. Ambrizzi (1993), Rossb wave roagation on a realistic longitudinall varing flow, J. Atomos. Sci., 50, Kurosaki, Y., and M. Mikami (2003), Recent frequent dust events and their relation to surface wind in East Asia, Geohs. Res. Lett., 30, 1736, doi: /2003 GL Morinaga, Y., and M. Shinoda (2003), Dzud the natural disaster in Mongolia, Sci. J. KAGAKU, 73, Nakamura, H., and T. Fukamachi (2004), Evolution and dnamics of summertime blocking over the Far East and the associated surface Okhotsk high, Quart. J. Ro. Meteor. Soc., 130, Nishii K., and H. Nakamura (2004), Lower-stratosheric Rossb wave trains in the southern hemishere: A case-stud for late winter of 1997, Quart. J. Ro. Meteor. Soc., 130, Pell, J.L., and B.J. Hoskins (2003), A new ersective on blocking, J. Atomos. Sci., 6, Sato, N., and M. Takahashi (2006), Dnamical rocesses related to the aearance of quasi-stationar waves on the subtroical jet in the midsummer Northern Hemishere, J. Climate, 19, Takaa K., and H. Nakamura (2001), A formulation of a hase-indeendent wave-activit flu for stationar and migrator quasigeostrohic eddies on a zonall varing basic flow, J. Atomos. Sci., 58, Terao (1998), Barotroic disturbances on intraseasonal time scales observed in the midlatitudes over the Eurasian continent during the northern summer, J. Meteor. Soc. Jaan, 76, UNEP (1997), World atlas of desertification. Second edition, edited b Middleton N.J. and Thomas D.S.G., Arnold, 182. Yatagai, A., and T. Yasunari (1995), Interannual variations of summer reciitation in the arid/semiarid regions in China and Mongolia: Their regionalit and relation to the Asian summer monsoon, J. Meteor. Soc. Jaan, 73,
No pp The Relationship between Southeast Asian Summer Monsoon and Upper Atmospheric Field over Eurasia Takeshi MORI and Shuji YAMAKAWA
No.42 2007 pp.159 166 The Relationship between Southeast Asian Summer Monsoon and Upper Atmospheric Field over Eurasia Takeshi MORI and Shuji YAMAKAWA Received September 30, 2006 Using Southeast Asian
More informationhPa ( ) hPa
200520241 19 1 18 1993 850hPa 6 7 6 27 7 3 6 29 ( ) 250 200hPa i iii 1 1 1.1...................................... 1 1.1.1................................. 1 1.1.2......................... 1 1.1.3...........
More information* Meso- -scale Features of the Tokai Heavy Rainfall in September 2000 Shin-ichi SUZUKI Disaster Prevention Research Group, National R
38 2002 7 2000 9 * Meso- -scale Features of the Tokai Heavy Rainfall in September 2000 Shin-ichi SUZUKI Disaster Prevention Research Group, National Research Institute for Earth Science and Disaster Prevention,
More information19982004 7 1998 2004 7 1.2.1 1.2.2 1.2.1 7 1.2.2 1.1.3 1.2.2 1.2.3 7 2.1.1 1998 19982004 7 125 2000 8 3 34 46 1.3.3 1980 1900 7 1900 7 7 19981999 1998200020032004 2003 1.2.3 10 35 1998 2001 2000 1112 19982004
More information宮本大輔 山川修治
No.53 2018 pp.163 175 PDO The Relationships between Pacific Decadal Oscillation (PDO) and Synoptic Climate System Daisuke MIYAMOTO and Shuji YAMAKAWA Accepted November 30, 2017 We investigated the relationships
More information1 flux flux Plumb (1985) flux F s Plumb (1985) Karoly et al. (1989) flux flux Plumb (1985) Plumb (1986) Trenberth (1986) Andrews (1983) review flux Pl
wave-activity flux flux flux ( ) E-mail: takaya@jamstec.go.jp 1 Introduction ( ) (e.g., Nakamura et al. 1997) storm track cyclogenesis downstream development (e.g., Chang 1993) wave-activity ( ) flux (
More information, 1.,,,.,., (Lin, 1955).,.,.,.,. f, 2,. main.tex 2011/08/13( )
81 4 2 4.1, 1.,,,.,., (Lin, 1955).,.,.,.,. f, 2,. 82 4.2. ζ t + V (ζ + βy) = 0 (4.2.1), V = 0 (4.2.2). (4.2.1), (3.3.66) R 1 Φ / Z, Γ., F 1 ( 3.2 ). 7,., ( )., (4.2.1) 500 hpa., 500 hpa (4.2.1) 1949,.,
More information85 4
85 4 86 Copright c 005 Kumanekosha 4.1 ( ) ( t ) t, t 4.1.1 t Step! (Step 1) (, 0) (Step ) ±V t (, t) I Check! P P V t π 54 t = 0 + V (, t) π θ : = θ : π ) θ = π ± sin ± cos t = 0 (, 0) = sin π V + t +V
More informationMicrosoft Word - ijou.doc
夏季アジアモンスーンに伴う対流圏 - 成層圏循環の変動 井上誠 高橋正明 ( 東大 CCSR) 1. はじめに成層圏と対流圏の関連性を論じた研究には 北半球冬季に関するものが多い 例えば,Boville(1984) は 大気大循環モデルを使って 成層圏極夜ジェットの変化が対流圏にまで及ぶことを示した また Niwano and Takahashi(1998) は QBO と対流圏中高緯度大循環との関係を大気大循環モデルで解析した
More information() 1 1 2 2 3 2 3 308,000 308,000 308,000 199,200 253,000 308,000 77,100 115,200 211,000 308,000 211,200 62,200 185,000 308,000 154,000 308,000 2 () 308,000 308,000 253,000 308,000 77,100 211,000 308,000
More information128 3 II S 1, S 2 Φ 1, Φ 2 Φ 1 = { B( r) n( r)}ds S 1 Φ 2 = { B( r) n( r)}ds (3.3) S 2 S S 1 +S 2 { B( r) n( r)}ds = 0 (3.4) S 1, S 2 { B( r) n( r)}ds
127 3 II 3.1 3.1.1 Φ(t) ϕ em = dφ dt (3.1) B( r) Φ = { B( r) n( r)}ds (3.2) S S n( r) Φ 128 3 II S 1, S 2 Φ 1, Φ 2 Φ 1 = { B( r) n( r)}ds S 1 Φ 2 = { B( r) n( r)}ds (3.3) S 2 S S 1 +S 2 { B( r) n( r)}ds
More informationHolton semigeostrophic semigeostrophic,.., Φ(x, y, z, t) = (p p 0 )/ρ 0, Θ = θ θ 0,,., p 0 (z), θ 0 (z).,,,, Du Dt fv + Φ x Dv Φ + fu +
Holton 9.2.2 semigeostrophic 1 9.2.2 semigeostrophic,.., Φ(x, y, z, t) = (p p 0 )/ρ 0, Θ = θ θ 0,,., p 0 (z), θ 0 (z).,,,, Du Dt fv + Φ x Dv Φ + fu + Dt DΘ Dt + w dθ 0 dz = 0, (9.2) = 0, (9.3) = 0, (9.4)
More information陸域環境研究センター
No.53 12 2004 Palmer Drought Severity Index PDSI An Analysis of Drought in Mongolia Using Palmer Drought Severity Index PDSI * ** Kazumi SUZUKI * and Tsutomu YAMANAKA ** 2002 1951 1990 Yatagai and Yasunari,
More information1. 4cm 16 cm 4cm 20cm 18 cm L λ(x)=ax [kg/m] A x 4cm A 4cm 12 cm h h Y 0 a G 0.38h a b x r(x) x y = 1 h 0.38h G b h X x r(x) 1 S(x) = πr(x) 2 a,b, h,π
. 4cm 6 cm 4cm cm 8 cm λ()=a [kg/m] A 4cm A 4cm cm h h Y a G.38h a b () y = h.38h G b h X () S() = π() a,b, h,π V = ρ M = ρv G = M h S() 3 d a,b, h 4 G = 5 h a b a b = 6 ω() s v m θ() m v () θ() ω() dθ()
More information警察も変わった。企業にできないはずがない, If Cops Can Change, So Can Corporations, 「ピープル・ビジネス」の新ルール, New Rules for People Business
More information
キラッ都ナゴヤ10月号 _cs5.indd
祭 イベント6 1 - http://www.nagoyameshi-expo.com/ 2, 3 1 - - http://www.osuengei.nagoya/ 4235 1 - http://www.wfg-bluebonnet.com/ PR 4235 1 - http://www.higashiyama.city.nagoya.jp イベント 3 1-2, 3 1-3 1 423 6 1
More information26 11 20 H20,H25 26 11 20 9 2014in (H24) 9 2014in (H2223,25) 34 (H2223,25) 9 2014in 26 11 20 9 2014in (H2223) (H2223,25) HAPPY 9 2014in (H2225) 5 6 50kg 60kg 17 6 50kg 60kg 71 1 1415 50kg 26 11 20 9 2014in
More informationNote.tex 2008/09/19( )
1 20 9 19 2 1 5 1.1........................ 5 1.2............................. 8 2 9 2.1............................. 9 2.2.............................. 10 3 13 3.1.............................. 13 3.2..................................
More information140 120 100 80 60 40 20 0 115 107 102 99 95 97 95 97 98 100 64 72 37 60 50 53 50 36 32 18 H18 H19 H20 H21 H22 H23 H24 H25 H26 H27 1 100 () 80 60 40 20 0 1 19 16 10 11 6 8 9 5 10 35 76 83 73 68 46 44 H11
More information支持力計算法.PDF
. (a) P P P P P P () P P P P (0) P P Hotω H P P δ ω H δ P P (a) ( ) () H P P n0(k P 4.7) (a)0 0 H n(k P 4.76) P P n0(k P 5.08) n0(k P.4) () 0 0 (0 ) n(k P 7.56) H P P n0(k P.7) n(k P.7) H P P n(k P 5.4)
More information1
1 450 2 3 .113 4 5 19 1850 1852 1854 1855 1857 1864 1867 1868 1863 64 1854 1855 1857 1861 1854 6 1861 1863 1865 6 1855 1857 50 7 8 9 1880 1872 1894 700 1893 1894 1896 700 1895 4 1,600 1898 6,200 20 19,000
More informationMicrosoft Word 成果報告書.doc
22-1213-004 22 2010 6 7 7 20, 2010;, 2010 e.g., Keefer and Larsen, 2007; Larsen et al., 2010 Wieczorek and Glade, 2005 e.g., Onodera et al., 1974; Keefer et al., 1987; Saito et al., 2010a 1984Soil Water
More information0946: : : :30 UT 1004:30 UT global expansion global expansion pseudo breakup pseudo breakup 3 1: Kotzebue UT [Sh
[ : ( ) ] 1 1957 1958 IGY (International Geophysical Year) 2007 THEMIS NASA 20 MTI c Mesosphere Thermosphere Ionosphere (MTI) Research Group, Japan 2 IGY [Feldstein, 1963] 75 65 Akasofu [1964] Akasofu
More informationQCD 1 QCD GeV 2014 QCD 2015 QCD SU(3) QCD A µ g µν QCD 1
QCD 1 QCD GeV 2014 QCD 2015 QCD SU(3) QCD A µ g µν QCD 1 (vierbein) QCD QCD 1 1: QCD QCD Γ ρ µν A µ R σ µνρ F µν g µν A µ Lagrangian gr TrFµν F µν No. Yes. Yes. No. No! Yes! [1] Nash & Sen [2] Riemann
More information63 3.2,.,.,. (2.6.38a), (2.6.38b), V + V V + Φ + fk V = 0 (3.2.1)., Φ = gh, f.,. (2.6.40), Φ + V Φ + Φ V = 0 (3.2.2). T = L/C (3.2.3), C. C V, T = L/V
62 3 3.1,,.,. J. Charney, 1948., Burger(1958) Phillips(1963),.,. L : ( 1/4) T : ( 1/4) V :,. v x u x V L, etc, u V T,,.,., ( )., 2.1.1. 63 3.2,.,.,. (2.6.38a), (2.6.38b), V + V V + Φ + fk V = 0 (3.2.1).,
More information: (1:, 2:, 3:, 4: ) 1 (Stratospheric Sudden Warming; SSW),, 1 (Displacement), 2 (Splitting) 2 (Charlton and Polvani 2007)., (Mi
: 2009 1 1 2 3 3 4 3 3 3 (1:, 2:, 3:, 4: ) 1 (Stratospheric Sudden Warming; SSW),, 1 (Displacement), 2 (Splitting) 2 (Charlton and Polvani 2007)., (Mitchell et al. 2013),. SSW,, (Labitzke 1965),, SSW,,
More information120 9 I I 1 I 2 I 1 I 2 ( a) ( b) ( c ) I I 2 I 1 I ( d) ( e) ( f ) 9.1: Ampère (c) (d) (e) S I 1 I 2 B ds = µ 0 ( I 1 I 2 ) I 1 I 2 B ds =0. I 1 I 2
9 E B 9.1 9.1.1 Ampère Ampère Ampère s law B S µ 0 B ds = µ 0 j ds (9.1) S rot B = µ 0 j (9.2) S Ampère Biot-Savart oulomb Gauss Ampère rot B 0 Ampère µ 0 9.1 (a) (b) I B ds = µ 0 I. I 1 I 2 B ds = µ 0
More information2. 2 P M A 2 F = mmg AP AP 2 AP (G > : ) AP/ AP A P P j M j F = n j=1 mm j G AP j AP j 2 AP j 3 P ψ(p) j ψ(p j ) j (P j j ) A F = n j=1 mgψ(p j ) j AP
1. 1 213 1 6 1 3 1: ( ) 2: 3: SF 1 2 3 1: 3 2 A m 2. 2 P M A 2 F = mmg AP AP 2 AP (G > : ) AP/ AP A P P j M j F = n j=1 mm j G AP j AP j 2 AP j 3 P ψ(p) j ψ(p j ) j (P j j ) A F = n j=1 mgψ(p j ) j AP
More informationTaro13-①表紙関係.jtd
39 03 04 05 -- -2- ?? A A D = A B C A2 HI H = DG BC B = A G = EF C E = A I = H F = AE -39- 2 3 0.8 n n n n n 0.8 n n 0.8 n 70 30 00 70 30 70 30 00 250 250 200 bn 400
More information第2章
2 IPCC SRES 2.1 1 2000 3 15 IPCC 1990 1992 IPCC 8 IPCC 1992 Houghton et al, 1992 IS92aIPCC 1992 a 6 1985 1990 1990 1992 1994 IPCC Alcamo et al, 1994 IPCC 1996 IPCC IPCC 3 IPCC IPCC 3 3 IPCC 3 Special Report
More information% 4.4% % 5.0% % 4.5% % 2.7% % 2.0% % 3.6% 5.1% 4.5% 2.6% 3.6%
11 10 12 8.9% 4.4% 2005 9.2% 5.0% 2006 6.5% 4.5% 2007 1.0% 2.7% 2008 1.9% 2.0% 2009 7.3% 3.6% 5.1% 4.5% 2.6% 3.6% 2012 2011 2010 2004 H22.3.27 2011 3 10 2010 9 10 2 128 60 191041 100 100 2011 JR km 89
More informationたたら製鉄についてのまとめ
65 1229 1570 5 3 5 2769 1876 1889 9 1892 1927-73 - - 1619 131 2 5500 43 194 1889 1955-1617 3 2 3 1186 2 9 15 1165-74 - 596 300 200 4 888 4 888 11 3 8892 10 2 969 708781782888 729 749 859 877 3 947 3 1523
More informationmeiji_resume_1.PDF
β β β (q 1,q,..., q n ; p 1, p,..., p n ) H(q 1,q,..., q n ; p 1, p,..., p n ) Hψ = εψ ε k = k +1/ ε k = k(k 1) (x, y, z; p x, p y, p z ) (r; p r ), (θ; p θ ), (ϕ; p ϕ ) ε k = 1/ k p i dq i E total = E
More informationSRES 4 A1 A1B A1T A1FI A2 B1 B2 A1 B1 21 IS92a IPCC 1994 IPCC % IPCC IPCC 1996 SRES IS c SRES A2 B2 MRI2 / CCSR/NIES2 HadCM2 CGCM2
IPCC 2001 2.7.1 2.7.2 2.7.3 2.7.1 5 2.7.2 5 1.4 SRES Special Report on Emissions Scenarios IPCC, 2000 2.7.1 a SRES IS92 IPCC, 1994 2.7.1 b CH 4 N 2 O CFCs 2.7.1 c 2.6 223 IPCC 21 SRES 4 A1 A1B A1T A1FI
More informationmains.dvi
8 Λ MRI.COM 8.1 Mellor and Yamada (198) level.5 8. Noh and Kim (1999) 8.3 Large et al. (1994) K-profile parameterization 8.1 8.1: (MRI.COM ) Mellor and Yamada Noh and Kim KPP (avdsl) K H K B K x (avm)
More informationあさひ indd
2006. 0. 2 2006. 0. 4 30 8 70 2 65 65 40 65 62 300 2006. 0. 3 7 702 22 7 62802 7 385 50 7 385 50 8 385 50 0 2 390 526 4 2006. 0. 0 0 0 62 55 57 68 0 80 5000 24600 37200 0 70 267000 500000 600 2 70 70 267000
More informationNo δs δs = r + δr r = δr (3) δs δs = r r = δr + u(r + δr, t) u(r, t) (4) δr = (δx, δy, δz) u i (r + δr, t) u i (r, t) = u i x j δx j (5) δs 2
No.2 1 2 2 δs δs = r + δr r = δr (3) δs δs = r r = δr + u(r + δr, t) u(r, t) (4) δr = (δx, δy, δz) u i (r + δr, t) u i (r, t) = u i δx j (5) δs 2 = δx i δx i + 2 u i δx i δx j = δs 2 + 2s ij δx i δx j
More information取扱説明書 [F-02F]
F-02F 4. 2 3 4 5 6 7 8 9 0 2 3 4 5 6 7 8 a b c d a b c d a b cd 9 e a b c d e 20 2 22 ab a b 23 a b 24 c d e 25 26 o a b c p q r s t u v w d h i j k l e f g d m n a b c d e f g h i j k l m n x 27 o
More information修士論文
SAW 14 2 M3622 i 1 1 1-1 1 1-2 2 1-3 2 2 3 2-1 3 2-2 5 2-3 7 2-3-1 7 2-3-2 2-3-3 SAW 12 3 13 3-1 13 3-2 14 4 SAW 19 4-1 19 4-2 21 4-2-1 21 4-2-2 22 4-3 24 4-4 35 5 SAW 36 5-1 Wedge 36 5-1-1 SAW 36 5-1-2
More information2003 El Niño 0AOG1102
003 El Niño 0AOG0 El Niño El Niño El Niño ( ) El Niño event (997-98 00-03 ) OLR( ) 0-70 (CEOF) El Niño El Niño(00-003) El Niño 3 3-3- 3-- 3-- 4 5 (CEOF ) 6 7 7- OLR 7- El Niño event OLR 7-3 El Niño event
More informationA = A x x + A y y + A, B = B x x + B y y + B, C = C x x + C y y + C..6 x y A B C = A x x + A y y + A B x B y B C x C y C { B = A x x + A y y + A y B B
9 7 A = A x x + A y y + A, B = B x x + B y y + B, C = C x x + C y y + C..6 x y A B C = A x x + A y y + A B x B y B C x C y C { B = A x x + A y y + A y B B x x B } B C y C y + x B y C x C C x C y B = A
More informationall.dvi
38 5 Cauchy.,,,,., σ.,, 3,,. 5.1 Cauchy (a) (b) (a) (b) 5.1: 5.1. Cauchy 39 F Q Newton F F F Q F Q 5.2: n n ds df n ( 5.1). df n n df(n) df n, t n. t n = df n (5.1) ds 40 5 Cauchy t l n mds df n 5.3: t
More information1
1 1.. ( ) ( ) ( ) (A) E icb φ Et = + cdiva ct (H3) (B) ( ) ct ct ' ctct ' + ' = ' ct ' + ct ' i( ') (H3,H18) 3 (i) cosh Ψ = cosh ΘcoshΩ sinhψ sinhθ sinhω cosh Ψ cosh Θ cosh Ω = sinhψ sinhθ sinhω tanhψ
More information4) H. Takayama et al.: J. Med. Chem., 45, 1949 (2002). 5) H. Takayama et al.: J. Am. Chem. Soc., 112, 8635 (2000). 6) H. Takayama et al.: Tetrahedron Lett., 42, 2995 (2001). 9) M. Kitajima et al: Chem.
More information(1.2) T D = 0 T = D = 30 kn 1.2 (1.4) 2F W = 0 F = W/2 = 300 kn/2 = 150 kn 1.3 (1.9) R = W 1 + W 2 = = 1100 N. (1.9) W 2 b W 1 a = 0
1 1 1.1 1.) T D = T = D = kn 1. 1.4) F W = F = W/ = kn/ = 15 kn 1. 1.9) R = W 1 + W = 6 + 5 = 11 N. 1.9) W b W 1 a = a = W /W 1 )b = 5/6) = 5 cm 1.4 AB AC P 1, P x, y x, y y x 1.4.) P sin 6 + P 1 sin 45
More information2009 Aida et al. Caries Res 2006;40 2000 100 % 78.7 88.0 96.6 98.8 98.8 98.8 100.0 100.0 100 75 69.4 50 75.3 74.8 73.3 73.1 73.0 72.4 71.8 71.7 51.7 40.2 69.4 68.8 73.6 25 22.3 32.8 21.9 22.9 22.1
More informationV(x) m e V 0 cos x π x π V(x) = x < π, x > π V 0 (i) x = 0 (V(x) V 0 (1 x 2 /2)) n n d 2 f dξ 2ξ d f 2 dξ + 2n f = 0 H n (ξ) (ii) H
199 1 1 199 1 1. Vx) m e V cos x π x π Vx) = x < π, x > π V i) x = Vx) V 1 x /)) n n d f dξ ξ d f dξ + n f = H n ξ) ii) H n ξ) = 1) n expξ ) dn dξ n exp ξ )) H n ξ)h m ξ) exp ξ )dξ = π n n!δ n,m x = Vx)
More informationnsg02-13/ky045059301600033210
φ φ φ φ κ κ α α μ μ α α μ χ et al Neurosci. Res. Trpv J Physiol μ μ α α α β in vivo β β β β β β β β in vitro β γ μ δ μδ δ δ α θ α θ α In Biomechanics at Micro- and Nanoscale Levels, Volume I W W v W
More information液晶の物理1:連続体理論(弾性,粘性)
The Physics of Liquid Crystals P. G. de Gennes and J. Prost (Oxford University Press, 1993) Liquid crystals are beautiful and mysterious; I am fond of them for both reasons. My hope is that some readers
More information18 2 F 12 r 2 r 1 (3) Coulomb km Coulomb M = kg F G = ( ) ( ) ( ) 2 = [N]. Coulomb
r 1 r 2 r 1 r 2 2 Coulomb Gauss Coulomb 2.1 Coulomb 1 2 r 1 r 2 1 2 F 12 2 1 F 21 F 12 = F 21 = 1 4πε 0 1 2 r 1 r 2 2 r 1 r 2 r 1 r 2 (2.1) Coulomb ε 0 = 107 4πc 2 =8.854 187 817 10 12 C 2 N 1 m 2 (2.2)
More informationThe Physics of Atmospheres CAPTER :
The Physics of Atmospheres CAPTER 4 1 4 2 41 : 2 42 14 43 17 44 25 45 27 46 3 47 31 48 32 49 34 41 35 411 36 maintex 23/11/28 The Physics of Atmospheres CAPTER 4 2 4 41 : 2 1 σ 2 (21) (22) k I = I exp(
More information2012 年5 月6 日の竜巻の概要と竜巻リスク管理
NKSJ-RM 67 Jun Mizuta Shohei Hashimoto 2012 5 6 茨 2006 11 7 5 1. 5 6 1 1002hPa 25.8 5,500 24 2 1 5 6 12 1 2 5 6 9 5,500m 2 1,http://www.jma.go.jp/jma/menu/tatsumaki-portal/saigai-kishou.pdf:2012-05-11
More informationK E N Z U 01 7 16 HP M. 1 1 4 1.1 3.......................... 4 1.................................... 4 1..1..................................... 4 1...................................... 5................................
More information草津白根山における地磁気全磁力・自然電位観測
1 2 1 1 1 3 1 1 1 1 1 2 3 Observation of Geomagnetic Total Force and Self-potential at Kusatsu-Shirane Volcano T.Koike 1 I.Suganuma 2 T.Uesugi 1 I.Fujii 1 H.Takahashi 1 K.Ikeda 3 N.Kumasaka 1 T.Ookawa
More information( ( 3 ( ( 6 (
( ( ( 43037 3 0 (Nicolas Bourbaki (Éléments d'histoire des athématiques : 984 b b b n ( b n/b n b ( 0 ( p.3 3500 ( 3500 300 4 500 600 300 (Euclid (Eukleides : EÎkleÐdhc : 300 (StoiqeÐwsic 7 ( 3 p.49 (
More informationGauss Gauss ɛ 0 E ds = Q (1) xy σ (x, y, z) (2) a ρ(x, y, z) = x 2 + y 2 (r, θ, φ) (1) xy A Gauss ɛ 0 E ds = ɛ 0 EA Q = ρa ɛ 0 EA = ρea E = (ρ/ɛ 0 )e
7 -a 7 -a February 4, 2007 1. 2. 3. 4. 1. 2. 3. 1 Gauss Gauss ɛ 0 E ds = Q (1) xy σ (x, y, z) (2) a ρ(x, y, z) = x 2 + y 2 (r, θ, φ) (1) xy A Gauss ɛ 0 E ds = ɛ 0 EA Q = ρa ɛ 0 EA = ρea E = (ρ/ɛ 0 )e z
More informationX G P G (X) G BG [X, BG] S 2 2 2 S 2 2 S 2 = { (x 1, x 2, x 3 ) R 3 x 2 1 + x 2 2 + x 2 3 = 1 } R 3 S 2 S 2 v x S 2 x x v(x) T x S 2 T x S 2 S 2 x T x S 2 = { ξ R 3 x ξ } R 3 T x S 2 S 2 x x T x S 2
More information2/24
Dec. 18 20, 2006 in DEX-SMI 2006 DC http://www.smapip.is.tohou.ac.jp/ jun/ in collaboration with M. Yasuda and K. Tanaa 1/24 2/24 scientific papers scientists Glucose 2 Lactate 2 ATP 2-Triose-P 2 P 2 NAD
More information2000年度『数学展望 I』講義録
2000 I I IV I II 2000 I I IV I-IV. i ii 3.10 (http://www.math.nagoya-u.ac.jp/ kanai/) 2000 A....1 B....4 C....10 D....13 E....17 Brouwer A....21 B....26 C....33 D....39 E. Sperner...45 F....48 A....53
More information[1.1] r 1 =10e j(ωt+π/4), r 2 =5e j(ωt+π/3), r 3 =3e j(ωt+π/6) ~r = ~r 1 + ~r 2 + ~r 3 = re j(ωt+φ) =(10e π 4 j +5e π 3 j +3e π 6 j )e jωt
3.4.7 [.] =e j(t+/4), =5e j(t+/3), 3 =3e j(t+/6) ~ = ~ + ~ + ~ 3 = e j(t+φ) =(e 4 j +5e 3 j +3e 6 j )e jt = e jφ e jt cos φ =cos 4 +5cos 3 +3cos 6 =.69 sin φ =sin 4 +5sin 3 +3sin 6 =.9 =.69 +.9 =7.74 [.]
More informationτ τ
1 1 1.1 1.1.1 τ τ 2 1 1.1.2 1.1 1.1 µ ν M φ ν end ξ µ ν end ψ ψ = µ + ν end φ ν = 1 2 (µφ + ν end) ξ = ν (µ + ν end ) + 1 1.1 3 6.18 a b 1.2 a b 1.1.3 1.1.3.1 f R{A f } A f 1 B R{AB f 1 } COOH A OH B 1.3
More informationsakigake1.dvi
(Zin ARAI) arai@cris.hokudai.ac.jp http://www.cris.hokudai.ac.jp/arai/ 1 dynamical systems ( mechanics ) dynamical systems 3 G X Ψ:G X X, (g, x) Ψ(g, x) =:Ψ g (x) Ψ id (x) =x, Ψ gh (x) =Ψ h (Ψ g (x)) (
More information東海水害報告書最終版.PDF
2000 9 11 12 1 114 11 1 428 2 3 1 1 270 912 330 100 18,000 10 98 27 77 27,180 44,111 1.1.1. 8,500 1,000 4 5 9 9 11 5 20 4,234 11,130 6 2 8 7 15 1,703 9 12 25 297 7 606 7 30 264 24 222,651 579,451 1.1.2
More information2004 10 2004 1984 2 1986 4 20 60 1 3 1 1 1 13,300 2 2 2 3 1 2004 2009 2 1 1 2 1 1985 97JR JT NTT 2002 96 97 4 JR JT 97 3 JR 19 29 JT 2.4 2.5 JR JT NTT JR JT NTT 2 97 4 JR 20.09 JT 19.92 NTT 17.35 17.35
More information16 17 17 9 14 11 18 3 18 3 31 31 21 32 50 ( 160km) 130 42 131 53 ( 70km) 116 6 ( 0.92%) 7,735km 2 ( 2.05%) ( 14(2002)10 1 ) 14 76 80km 10 400km 4(1871)7 6 11 3 5(1872)9 14 6(1873)1 2 9(1876)8 16(1883)5
More information21 23 2 731 3 20 1946 1949 26 4 28 2 58 1984 3 1989 1 9 1995 163 175 1998 1 142 150 4 17 (1981 12 )
50 1 50 1 2 1999 3 21 23 2 731 3 20 1946 1949 26 4 28 2 58 1984 3 1989 1 9 1995 163 175 1998 1 142 150 4 17 (1981 12 ) 5 6 7 8 9 1956 10 1964 30 38 39 11 5 27 32 1956 6 60 6 1965 13 1973 9 223 257 19 1975
More information( ) ) ) ) 5) 1 J = σe 2 6) ) 9) 1955 Statistical-Mechanical Theory of Irreversible Processes )
( 3 7 4 ) 2 2 ) 8 2 954 2) 955 3) 5) J = σe 2 6) 955 7) 9) 955 Statistical-Mechanical Theory of Irreversible Processes 957 ) 3 4 2 A B H (t) = Ae iωt B(t) = B(ω)e iωt B(ω) = [ Φ R (ω) Φ R () ] iω Φ R (t)
More information研究室ガイダンス(H28)福山研.pdf
1 2 3 4 5 4 He M. Roger et al., JLTP 112, 45 (1998) A.F. Andreev and I.M. Lifshitz, Sov. Phys. JETP 29, 1107 (1969) Born in 2004 (hcp 4 He) E. Kim and M.H.W. Chan, Nature 427, 225 (2004); Science 305,
More information目 次 受 賞 者 紹 介 スーザン ソロモン 博 士... 1 記 念 講 演 オゾン 層 破 壊 と 気 候 変 動 : 極 から 極 へ 単 独 旅 行... 3 受 賞 者 紹 介 グロ ハルレム ブルントラント 博 士... 117 記 念 講 演 持 続 可 能 な 開 発 に 向 け
平 成 16 年 度 ( 第 13 回 )ブループラネット 賞 受 賞 者 記 念 講 演 会 THE ASAHI GLASS FOUNDATION 目 次 受 賞 者 紹 介 スーザン ソロモン 博 士... 1 記 念 講 演 オゾン 層 破 壊 と 気 候 変 動 : 極 から 極 へ 単 独 旅 行... 3 受 賞 者 紹 介 グロ ハルレム ブルントラント 博 士... 117 記 念
More informationnote1.dvi
(1) 1996 11 7 1 (1) 1. 1 dx dy d x τ xx x x, stress x + dx x τ xx x+dx dyd x x τ xx x dyd y τ xx x τ xx x+dx d dx y x dy 1. dx dy d x τ xy x τ x ρdxdyd x dx dy d ρdxdyd u x t = τ xx x+dx dyd τ xx x dyd
More informationMilnor 1 ( ), IX,. [KN].,. 2 : (1),. (2). 1 ; 1950, Milnor[M1, M2]. Milnor,,. ([Hil, HM, IO, St] ).,.,,, ( 2 5 )., Milnor ( 4.1)..,,., [CEGS],. Ω m, P
Milnor 1 ( ), IX,. [KN].,. 2 : (1),. (2). 1 ; 1950, Milnor[M1, M2]. Milnor,,. ([Hil, HM, IO, St] ).,.,,, ( 2 5 )., Milnor ( 4.1)..,,., [CEGS],. Ω m, PC ( 4 5 )., 5, Milnor Milnor., ( 6 )., (I) Z modulo
More information50 2 I SI MKSA r q r q F F = 1 qq 4πε 0 r r 2 r r r r (2.2 ε 0 = 1 c 2 µ 0 c = m/s q 2.1 r q' F r = 0 µ 0 = 4π 10 7 N/A 2 k = 1/(4πε 0 qq
49 2 I II 2.1 3 e e = 1.602 10 19 A s (2.1 50 2 I SI MKSA 2.1.1 r q r q F F = 1 qq 4πε 0 r r 2 r r r r (2.2 ε 0 = 1 c 2 µ 0 c = 3 10 8 m/s q 2.1 r q' F r = 0 µ 0 = 4π 10 7 N/A 2 k = 1/(4πε 0 qq F = k r
More information1 1.1,,,.. (, ),..,. (Fig. 1.1). Macro theory (e.g. Continuum mechanics) Consideration under the simple concept (e.g. ionic radius, bond valence) Stru
1. 1-1. 1-. 1-3.. MD -1. -. -3. MD 1 1 1.1,,,.. (, ),..,. (Fig. 1.1). Macro theory (e.g. Continuum mechanics) Consideration under the simple concept (e.g. ionic radius, bond valence) Structural relaxation
More informationxyz,, uvw,, Bernoulli-Euler u c c c v, w θ x c c c dv ( x) dw uxyz (,, ) = u( x) y z + ω( yz, ) φ dx dx c vxyz (,, ) = v( x) zθ x ( x) c wxyz (,, ) =
,, uvw,, Bernoull-Euler u v, w θ dv ( ) dw u (,, ) u( ) ω(, ) φ d d v (,, ) v( ) θ ( ) w (,, ) w( ) θ ( ) (11.1) ω φ φ dθ / dφ v v θ u w u w 11.1 θ θ θ 11. vw, (11.1) u du d v d w ε d d d u v ω γ φ w u
More information6kg 1.1m 1.m.1m.1 l λ ϵ λ l + λ l l l dl dl + dλ ϵ dλ dl dl + dλ dl dl 3 1. JIS 1 6kg 1% 66kg 1 13 σ a1 σ m σ a1 σ m σ m σ a1 f f σ a1 σ a1 σ m f 4
35-8585 7 8 1 I I 1 1.1 6kg 1m P σ σ P 1 l l λ λ l 1.m 1 6kg 1.1m 1.m.1m.1 l λ ϵ λ l + λ l l l dl dl + dλ ϵ dλ dl dl + dλ dl dl 3 1. JIS 1 6kg 1% 66kg 1 13 σ a1 σ m σ a1 σ m σ m σ a1 f f σ a1 σ a1 σ m
More information90 37 20 1439 09 1 1899 1917 1925 1999 1997 2009 2009 38 70 80 90 21 2008 2 Web 21 11 28 4,402 246,847 39 20 1929 J M 1936 3 2009 10 20 4 1998 14.5% 2001 15.3% 2004 14.9% 2007 15.7% 2000 OECD 10.6 14.9
More informationTakeshi Kudo 1, Yukihiro Takahashi 1, Mitsuteru Sato 1, Taishi Yamada 1, Nui Kobayashi 1, Yusuke Sanmiya 1, Tomohiro Inoue 2, H C Stenbaek- Nielsen 3,
Takeshi Kudo 1, Yukihiro Takahashi 1, Mitsuteru Sato 1, Taishi Yamada 1, Nui Kobayashi 1, Yusuke Sanmiya 1, Tomohiro Inoue 2, H C Stenbaek- Nielsen 3, Ma@hew G McHarg 4, Ryan K Haaland 5, Takeshi Kammae
More information<32322D8EA D89CD8D8797B294C E8A968388DF814589C193A1899B E5290EC8F438EA12D966B8A4393B98F5C8F9F926E95FB82CC8BC7926E F5
No.432008pp.287 302 Climatological Characteristics of Local Wind in the Tokachi District, Hokkaido, JAPAN Takashige KAWAI, Mai NAKAJYO, Hisashi KATO and Shuji YAMAKAWA Received September 30, 2007 Climatological
More information12 13 10 1 12 18 12 12 18 13 10 13 11 1 18 8 21 14:0016:00 H12 18 9 21 9:0010:30 3 4 19 2 23 13:3016:00 19 3 6 () 12:0013:00 2 (a)(b) (c) (a)(b)(c) (b)(c) (a) (a) 3 17 11 (1) (2) (3) (4) 578mm 51 6 17
More information1
10 2 1990 5 1993 6 16 11 24 18 35 1960 41 1966 19 2 11 14 30 1955 10 41 1966 12 16 45 40 35 2004 2004 2004 30 25 20 15 10 5 0 1950 1960 1970 1980 1990 2000 6 10 1 6 46 10 2223 2 6 10 6 10 1 6 7 8 1011
More information梅雨 秋雨の対比とそのモデル再現性 将来変化 西井和晃, 中村尚 ( 東大先端研 ) 1. はじめに Sampe and Xie (2010) は, 梅雨降水帯に沿って存在する, 対流圏中層の水平暖気移流の梅雨に対する重要性を指摘した. すなわち,(i) 初夏に形成されるチベット高現上の高温な空気塊
Title 梅雨 秋雨の対比と気候モデルによる再現性 将来変化 Author(s) 西井, 和晃 ; 中村, 尚 Citation 週間及び1か月予報における顕著現象の予測可能性 (2013): 236-239 Issue Date 2013-03 URL http://hdl.handle.net/2433/173472 Right Type Article Textversion publisher
More informationNCA1-V6-650 C9A1-V6-650
NCA1-V6-650 C9A1-V6-650 1 2 3 1 1 1 1 1 1 2 c 2 1 c 1 2 1 2 c 3 4 1 2 3 2 1 2 3 4 1 1 1 2 1 2 3 1 1 1 2 1 i u 1 2 3 o u i 4 o 4 5 1 2 o 1 o 1 o o 3 2 1 1 1 1 1 2 3 4 5 6 4 1
More informationOM Z49-A
NCA3 V6 650 C9A3 V6 650 1 2 3 1 1 1 1 2 c 1 1 2 1 2 1 1 c 2 c 3 4 1 2 3 1 2 3 4 1 2 1 1 2 1 3 2 1 1 1 2 1 i u 2 3 o u i 1 4 4 o o 1 o o 1 2 o 3 3 1 2 5 1 1 1 1 1 2 3 4 5 6
More informationuntitled
1 17 () BAC9ABC6ACB3 1 tan 6 = 3, cos 6 = AB=1 BC=2, AC= 3 2 A BC D 2 BDBD=BA 1 2 ABD BADBDA ABC6 BAD = (18 6 ) / 2 = 6 θ = 18 BAD = 12 () AD AD=BADCAD9 ABD ACD A 1 1 1 1 dsinαsinα = d 3 sin β 3 sin β
More information1. ( ) 1.1 t + t [m]{ü(t + t)} + [c]{ u(t + t)} + [k]{u(t + t)} = {f(t + t)} (1) m ü f c u k u 1.2 Newmark β (1) (2) ( [m] + t ) 2 [c] + β( t)2
212 1 6 1. (212.8.14) 1 1.1............................................. 1 1.2 Newmark β....................... 1 1.3.................................... 2 1.4 (212.8.19)..................................
More informationQUARTERLY JOURNAL HYDROGRAPHY Establishing a JCG/UKHO cooperative framework on nautical charts -- Part. (p. ), Investigations on reproduced Ino-zu Maps, Japanese historical maps,owned by JHOD.(p. ), Various
More information2009 I 2 II III 14, 15, α β α β l 0 l l l l γ (1) γ = αβ (2) α β n n cos 2k n n π sin 2k n π k=1 k=1 3. a 0, a 1,..., a n α a
009 I II III 4, 5, 6 4 30. 0 α β α β l 0 l l l l γ ) γ αβ ) α β. n n cos k n n π sin k n π k k 3. a 0, a,..., a n α a 0 + a x + a x + + a n x n 0 ᾱ 4. [a, b] f y fx) y x 5. ) Arcsin 4) Arccos ) ) Arcsin
More informationMacdonald, ,,, Macdonald. Macdonald,,,,,.,, Gauss,,.,, Lauricella A, B, C, D, Gelfand, A,., Heckman Opdam.,,,.,,., intersection,. Macdona
Macdonald, 2015.9.1 9.2.,,, Macdonald. Macdonald,,,,,.,, Gauss,,.,, Lauricella A, B, C, D, Gelfand, A,., Heckman Opdam.,,,.,,., intersection,. Macdonald,, q., Heckman Opdam q,, Macdonald., 1 ,,. Macdonald,
More information2009 IA 5 I 22, 23, 24, 25, 26, (1) Arcsin 1 ( 2 (4) Arccos 1 ) 2 3 (2) Arcsin( 1) (3) Arccos 2 (5) Arctan 1 (6) Arctan ( 3 ) 3 2. n (1) ta
009 IA 5 I, 3, 4, 5, 6, 7 6 3. () Arcsin ( (4) Arccos ) 3 () Arcsin( ) (3) Arccos (5) Arctan (6) Arctan ( 3 ) 3. n () tan x (nπ π/, nπ + π/) f n (x) f n (x) fn (x) Arctan x () sin x [nπ π/, nπ +π/] g n
More information