Nature ࡟⤂௓ࡉࢀࡓᑎ⏣ᐥᙪࡢㄽᩥ(1)኱᳃ ୍ᙪᐥ ᙪ ඛ ⏕ ࡢ ࠾ ᘵᏊ ࡢ୰ ㇂ Ᏹ ྜྷ 㑻 ࡣ , ඛ⏕ ࡢ◊ ✲ ᴗ ⦼ ࡟ ࡩ ࢀ ,ࠕ ⱥ ᅜࡢ ⛉ Ꮫ 㞧 ㄅ ࢿ ࣮ ࢳࣗ ࢔ㄅ(Nature) ࡟, ୡ⏺ࡢ┠ࡰࡋ࠸◊✲ࢆẖᅇᑡᩘ࡙࢏ᣠࡗ࡚⤂௓ࡋ࡚ࢄࡿ୰࡟, ඛ⏕ࡢ◊✲ࡀࢃࡀᅜ࠿ࡽࡣ୍␒ከࡃ⤂௓ࡉࢀ࡚ࢄࡓࡸ࠺࡛࠶ࡿࠖ̾ ࡜㏙࡭࡚࠸ࡿ.
㸡୰㇂㸸ࠕᩥ໬ྐୖࡢᑎ⏣ᐥᙪඛ⏕ࠖ.ࠗ෤ࡢ⳹࠘. ᒾἼ᭩ᗑ. 1938. p. 271ࠥ278.

ᐇ㝿࡟࠶ࡓࡗ࡚ࡳࡿ࡜, ௚ࡢ᪥ᮏே◊✲⪅ࡢྡ๓ࡶᩓぢࡍࡿࡀ, ᑎ⏣ࡣ 22 ௳ࡶ࠶ࡾഔฟࡋ࡚࠸ࡿ.୰
㇂ࡢப࠺࡜࠾ࡾࡔ. ࡛ࡣ, ᑎ⏣ࡢ࡝࠺࠸࠺ㄽᩥࡀྲྀࡾୖࡆࡽࢀ⤂௓ࡉࢀࡓ࠿, ㄪᰝ⤖ᯝࢆ, Nature ࡢⓎ⾜ᖺ᭶㡰࡟, ௨ୗࡢせ㡿࡛グࡍ.
A㸸Nature ㄅୖ࡟࠾ࡅࡿᑎ⏣ㄽᩥ⤂௓グ஦ࡢ᭩ㄅࢹ࣮ࢱ (ࢱ࢖ࢺࣝ. ᕳྕ. Ⓨ⾜ᖺ᭶᪥. ࣮࣌ࢪ).
B㸸⤂௓ࡉࢀࡓᑎ⏣ࡢㄽᩥࡢ᭩ㄅࢹ࣮ࢱ (ⴭ⪅㹙ඹⴭ⪅㹛. ࢱ࢖ࢺࣝ. ㄅྡ. ᕳྕ. Ⓨ⾜ᖺ᭶. ࣮࣌ࢪ).
㹙ㄽᩥ no. 㹛(ࠗᑎ⏣ᐥᙪ඲㞟 ⛉Ꮫ⠍࠘㹙Scientific Papers㹛཰㘓ㄽᩥ࡟௜୚ࡉࢀ࡚࠸ࡿ␒ྕ).

C㸸Nature ㄅࡢ⤂௓グ஦࠿ࡽࡢ୍㒊ᘬ⏝ (ཎᩥࡢࡲࡲ).
D㸸ཧ⪃᝟ሗ (ᙜヱㄽᩥࡢゎㄝ, ホ౯࡞࡝㸭㐺ษ࡞ᩥ⊩ࡀぢᙜࡓࡽ࡞࠸ሙྜࡣ✵ḍࡢࡲࡲ).

‫ڦ‬1. 㘒ど.
A. 㹙Optical Illusion㹛. Nature. Vol. 70, No. 1805. 1904. 6. 2. p. 107.
B. T. Terada㸸
㹙Optical Illusion㹛. ฟ∧ࡉࢀࡓㄽᩥࡢ⤂௓࡛ࡣ࡞ࡃ, ⦅㞟⪅࠶࡚ࡢ Letter ࡢ⤂௓࡛࠶ࡿ.
C. ࠕMr. T. Terada writes to us from the College of Science, Tokyo, to direct attention to an opticalillusion observed when lycopodium powder strewn on the surface of water is made to gyrate by a jet ofair. After the whirling powder has been fixedly regarded for some time, and the eyes are directed to an
adjoining table, the surface of the table appears to move in a direction contrary to that of thelycopodiumࠖ.
Dï1.

⏕⌮ගᏛⓗ⌧㇟ࢆぢ࠸ࡔࡋࡓᑎ⏣ࡢ, Nature ⦅㞟⪅࠶࡚ࡢሗ࿌ࡀࠑNotesࠒḍ࡟⤂௓ࡉࢀࡿ. ᑎ⏣㛛ୗࡢ⏣ᖾᙪኴ㑻ࡢゎㄝࢆᘬࡃ.ࠕ▼ᯇᏊࡢ⢊ࢆỈ㠃࡟ᩓᕸࡋࡇࢀ࡟✵Ẽࡢ jet ࢆᩳࡵ࡟྿ࡁ௜ࡅ࡚ࡸࡿ࡜,⢊ࡣ⾲㠃ࡢỈ࡜ඹ࡟ὶࢀ࡚⨾ࡋ࠸⦤ᶍᵝࢆ⏬ࡃ. ▖ࢆ⢊࠿ࡽᛴ࡟ࡑࡢࢸ࣮ࣈࣝࡢୖ࡟ⴠࡍ࡜, ࡇࢇ࡝ࡣࢸ࣮ࣈࣝࡢ㠃ࡀ⢊࡜ࡣ཯ᑐࡢྥ࡟㉮ࡿࡸ࠺࡟ࡳ࠼ࡿࠖ(⏣ᖾ㸸ࠕ⏕⌮ගᏛⓗ⌧㇟ࠖ.ࠗᛮ᝿࠘. 166 ྕ. 1936. 3.

p.

116ࠥ120).
Dï2.

኱ᒣ ṇࡣ, ᑎ⏣ࡢ㘒ど◊✲ࡢ⌧௦ⓗホ౯ࢆヨࡳ࡚࠸ࡿ.ࠕึᮇࡢ◊✲࡛ࡣ, Ỉ㠃ࡢ⦤ࡢືࡁࢆほᐹࡋࡘ࡙ࡅࡓᚋ, ┠ࢆ࡯࠿ࡢ᪉ྥ࡟ྥࡅࡿ࡜, Ṇࡗ࡚࠸ࡿࡣࡎࡢ㠃࡟, Ỉ㠃ࡢືࡁ࡜㏫᪉ྥࡢືࡁࡀ⏕ࡌࡿࡇ࡜ࢆ࡜ࡾୖࡆ࡚࠸ࡿࡀ, ࡇࢀࡣ㐠ືṧീ࡜࠿⁪ࡢ㘒ぬ࡜࿧ࡤࢀ, 19 ୡ⣖୰ⴥ࠿ࡽ⏕⌮Ꮫ⪅ࡸᚰ⌮Ꮫ⪅ࡢ㛫࡛ࡣ▱ࡽࢀࡓ⌧㇟࡛࠶ࡾ, ௒᪥࡛ࡣ኱⬻どぬ㔝ࡢ㐠ື᳨ฟᶵᵓࡢ㡰ᛂ࡛ㄝ᫂ࡉࢀ࡚࠸ࡿ. ࡲࡓ, ᅇ㌿ࡍࡿᡪ㢼ᶵࡢ㔠ᒓࡢ⩚᰿ࡢ⫼ᚋ࡟Ⰽ࡙࠸ࡓᩬⅬࡀぢ࠼ࡿࡇ࡜ࡶሗ࿌ࡋ࡚࠸ࡿ㹙ㄽᩥ no. 23㹛. ࡇࢀࡣ, ࣇ࢙ࣄࢼ࣮ ௨᮶▱ࡽࢀ࡚࠸ࡿ୺ほⰍࡢ୍✀࡜᝿ീࡉࢀࡿࡀ, ᅇ㌿㏿ᗘ࡞࡝ࡢ᮲௳ࡀ୙࡛᫂, ṇ☜࡞ㄽホࡣ࡛ࡁ࡞࠸.
࠸ࡎࢀ࡟ࡏࡼ, ㄞࢇࡔࡾ⪺࠸ࡓ▱㆑࡛࡞ࡃ, ࡘࡡ࡟⮬ศ⮬㌟ࡢ┠࡛Ⓨぢࡋࡓࡇ࡜࡟ᩗពࢆ⾲ࡋࡓ࠸ࠖᒣ㸸ࠕどぬ◊✲࡜≀⌮Ꮫ⪅ࠖ.ࠗ⛉Ꮫ࠘. 66 ༹ 10 ྕ. 1996. 10.

(኱p. 756ࠥ758).

‫ڦ‬2. ₻ộࡢ๪᣺ື.
A. The Secondary Oscillation of Ocean Tides.

Nature. Vol. 78, No. 2020. 1908. 7. 16. p. 249ࠥ

250.
B. K. Honda, T. Terada, Y. Yoshida and D. Isitani㸸An Investigation on the Secondary Oscillationof Oceanic Tides. Journal of the College of Science, Tokyo Imperial University, Vol. 24. 1908. 3. p. i
ࠥϿ, 1ࠥ110.㹙ㄽᩥ no. 36㹛.
³³³. Publications of the Earthquakes Investigation Committee in Foreign Languages , Vol. 26B,1908.㹙ㄽᩥ no. 37㹛.
C. ࠕ«)URPWKLVLWDSSHDUHGWKDW the whole mass of water in the bay was in simultaneous oscillation inDVWDWLRQDU\ZDYHDQDORJRXVWRWKHVRXQGïZDYHLQDQRSHQRUJDQSLSHDQGWKDWWKHED\VHOHFWHGIURPthe multitudinous ocean waves of various period the particular one to which it was able to respond, and,
OLNHDUHVRQDWRUZLWKVRXQGïZDYHVPDJQLILHGDQGPDGHLWFRQVSLFXRXV7KLVFRQFOXVLRQZDVYHULILHGE\
H[SHULPHQWDOLQYHVWLJDWLRQ« ࠖ.
Dï1. ࡇࡢㄽᩥࡢ౯್ࡢ㧗ࡉࡣ, Nature ㄅୖ࡟࠾࠸࡚, ᅗධࡾ࡛ 2 ࣮࣌ࢪࡶࡢㄅ㠃ࢆࡉࡁ, ⤂௓ࡍࡿ࡜࠸࠺◚᱁ࡢᢅ࠸᪉࡟ࡼࡃ⌧ࢃࢀ࡚࠸ࡿ (ᮏ✏ᮎ࡟⦰ᑠࡋ࡚㌿㍕). ᑎ⏣㛛ୗࡢᏱ⏣㐨㝯ࡣ,ࠕKrümmel ࡞࡝ࡢእᅜࡢᾏὒᏛ᭩࡟ࠑ᪥ᮏேࡢᡂࡋ࡜ࡆࡓඃ⚽࡞◊✲ࠒ࡜㈹㈶, ᗈࡃᘬ⏝ࡉࢀࡓࠖ࡜グࡋࡓ (Ᏹ⏣㸸ࠗᾏὒ◊✲Ⓨ㐩ྐ࠘ࠑᾏὒ⛉Ꮫᇶ♏ㅮᗙ࣭⿵༹ࠒ. ᮾᾏ኱Ꮫฟ∧఍.
Dï2.

1978. p. 299ࠥ305).

Ᏹ⏣ࡢᣦ᦬㹙Dï1㹛ࢆ࠺ࡅ࡚኱᳃୍ᙪࡣ, Krümmel ࡢᮏࢆ᥈ࡋ࡚ࡳࡓ.

Otto Krümmel㸸Handbuch der Ozeanographie㹙ᾏὒᏛࣁࣥࢻࣈࢵࢡ㹛. Stuttgart, J. Engelhorns Nachf.
1911. xϽ + 766p. 㸡ᮾ໭኱Ꮫ㝃ᒓᅗ᭩㤋໭㟷ⴥᒣศ㤋ᡤⶶ.
࡜࠸࠺ᾈ℟࡞ᮏ࡛࠶ࡿ. ࠑ,ïϯ.

Stehende Wellenࠒ㹙ᐃᖖἼ㹛ࡢ❶ࡢ,p. 161ࠥ162 ࡜, p. 184ࠥ185 ࡢ2 ࠿ᡤ࡟, ࡇࡢㄽᩥࡀᘬ⏝ࡉࢀ, ᅗධࡾ࡛, ヲࡋࡃゎㄝࡉࢀ࡚࠸ࡿࡢࢆぢ࠸ࡔࡋࡓ.
Dï3.

᳝㈅༤⨾ࡣ,ࠕࡇࡢㄽᩥࡣ, ࡲࡇ࡜࡟ࡍࡈ࠸ㄽᩥ࡛, 1908 ᖺ࡟ࡗ࡚ࡋࡲࡗ࡚࠸ࡓ. ͐ ᮏከ, ᑎ⏣ࡽࡣ, ⌮ㄽィ⟬ࡢࡳ࡞ࡽࡎ,‴᣺ື࡟㛵ࡍࡿ࡯࡜ࢇ࡝ࡢࡇ࡜ࢆࡸࡢᶍᆺࢆసࡾ, ࡑࡇ࡟௵ពࡢἼࢆ᣺Ꮚࡢ⤌ྜࢃࡏ࡟ࡼࡗ࡚Ⓨ⏕ࡉࡏ࡚, ⌮ㄽࡢ᳨ドࢆ⾜ࡗ࡚࠸ࡲࡍ. ͐ ࡑࡋ࡚, ௵ពࡢᙧ≧ࡢ‴࡟ᑐࡋ࡚, ඹ᣺࿘ᮇࢆồࡵࡿᘧࢆᑟ࠸࡚, ⌮ㄽ࡜ᐇ㦂࡜ࡢ᳨ドࢆ⾜ࡗ࡚࠸ࡲࡍࠖ࡜㏙࡭ࡓ (᳝㈅㸸ࠕ␒እ᪥ᮏᅵᮌྐ (2) ᑎ⏣ᐥᙪࠖ.ࠗᅵᮌᏛ఍ㄅ࠘.
Dï4.

67 ༹ 11 ྕ. 1982. 10. p. 77).

ᑎ⏣㛛ୗࡢ୰㔝⊷ேࡣ, ࡇࡢㄽᩥ୰ࡢゝⴥࠑ㬆㛛ࡢ₻ὶࡣ, ࠶ࡓ࠿ࡶ㢼⍆⟶ࡢཱྀ࡟྿ࡁࡘࡅࡽࢀࡓẼὶ࡜ྠࡌ࡛, Ẽὶࡀ㢼⍆⟶ෆ࡟Ẽᰕࡢᐃᖖ᣺ືࢆࡦࡁ㉳ࡇࡍ࡜ྠࡌࡃ, ኴᖹὒ࠿ࡽ᧛☻ℿ࡟ྥ࠿ࡗ࡚✺㐍ࡍࡿ₻ὶࡣ, ₻᠁‴ෆ࡟Ỉࡢᐃᖖ᣺ືࢆࡦࡁ㉳ࡇࡍࠒࢆᘬࡁ, ⴭ⪅ࡽࡢ⪃ᐹࢆヲࡋࡃゎㄝࡋࡓ(୰㔝㸸ࠗᾏࡢ ㄯヰᐊ࠘.
Dï5.

ㅮㄯ♫. 1970. p. 3ࠥ9).

ୖ⏣ ᑑࡣ, ㄽᩥ୰ࡢゝⴥࠑ‴࠶ࡿ࠸ࡣᾏࡢ୍㒊ศࡣὶయ᣺Ꮚࡢࡼ࠺࡟ᅛ᭷ࡢ᣺ື࿘ᮇ࡛᣺ືࡍࡿࠒࢆᘬࡁ, ࡇࡢ◊✲ࡢ⫼ᬒ, ⤒㐣, ព⩏࡟ࡘࡁヲࡋࡃゎㄝࡋࡓ(ୖ⏣㸸ࠕᑎ⏣ᐥᙪࡢ⛉Ꮫ㝶➹ࠖ.ࠗᵭ࠘(ᑎ⏣ᐥᙪグᛕ㤋཭ࡢ఍). ≉㞟ྕ. 1995. 5. p. 1ࠥ10).

‫ڦ‬3. 㘒ど.
A. 㹙Optical Illusion㹛. Nature. Vol. 78, No. 2020. 1908. 7. 16. p. 255.
B. T. Terada㸸
㹙Optical Illusion㹛. ฟ∧ࡉࢀࡓㄽᩥࡢ⤂௓࡛ࡣ࡞ࡃ, ⦅㞟⪅࠶࡚ࡢ Letter ࡢ⤂௓࡛࠶ࡿ.

C. ࠕ«$IWHUZDWFKLQJGURSVIDOOLQJDWWKHUDWHRIDERXWRQHDVHFRQGLQWRWKHFHQWUHRIDVPDOOSRRODQG
so causing circular ripples, he turned his eyes to a spot on a neighbouring bush. The bush appeared tocontract slowly towards the point looked at, but the contracting motion was slower than the diverging
motion of the ripples. A similar effect was noticed by looking at the ground or at wallࠖ.
³³³.

D.

‫ڦ‬4. ᆅ㟈Ἴࡢ㏿ᗘ.
A. Velocities of Earthquake Waves. Nature. Vol. 90, No. 2256. 1913. 1. 23. p. 579.
B. T. Terada㸸 2QWKH9HORFLW\RI6HDï:DYHV  Proc. Tokyo Math-Phys. Soc., Ser. ϩ, Vol. 6,No.

12. 1912. 6. p. 260ࠥ265.㹙ㄽᩥ no. 46㹛.
C. ࠕIn the Proceedings of the Tokyo Mathematico-Physical Society, Ͻ., 17,Mr. T. Terada considers theexperimental fact that the velocities of earthquake waves fall short of the values calculated byhydro-G\QDPLFDOPHWKRGV«7KHUHVXOWVVKRZWKDWWKHH[SODQDWLRQLVDSODXVLEOHRQH«ࠖ.
³³³.

D.

‫ڦ‬5. ᆅ㟈ࡢ㢖ᗘ࡜Ẽᅽࡢ໙㓄.
A. Seismic Frequency and Isobar Gradient. Nature. Vol. 95, No. 2382. 1915. 6. 24. p. 461.
B. T. Terada㸸On the Relation between Seismic Frequency and Isobar Gradient. Proc. Tokyo

Math-Phys. Soc., Ser. ϩ, Vol. 4, No. 22. 1908.[ ]. p. 454ࠥ459. 㹙ㄽᩥ no. 43㹛.
C.

ࠕ,QWKH3URFHHGLQJVRIWKH7RN\R0DWKHPDWLFRï3K\VLFDO6RFLHW\IRUDQG  3URI7HUDGD

and Dr. Hasegawa discussed the possibility of the barometric gradient over a region subject toearthquakes being one of the contributory caXVHVRIWKHLUSURGXFWLRQ« ࠖ.
Dï1.

ᑎ⏣ࡣ, ࡇࢀ࡜ྠෆᐜࡢㄽᩥࢆ࿴ᩥ࡛Ⓨ⾲ࡋ࡚࠸ࡿࡢ࡛, ୍㒊ᢒฟࡍࡿ (ᩥㄒᩥࢆཱྀㄒᩥ࡟᭩ࡁᨵࡵ,୍㒊ពヂࡋࡓ).ࠑᆅ㟈࡜Ẽᅽ࡜ࡢ㛵ಀ࡟ࡘ࠸࡚ࡢඛ⾜◊✲ࡣ࠶ࡿࡀ, ᆅ㟈࡜Ẽᅽࡢ໙㓄࡜ࡢ㛵ಀ࡟ࡘ࠸࡚ࡢヲ⣽࡞ㄪᰝࡣ࡞࠿ࡗࡓ. ᆅẆࡢᵓ㐀ࡣ」㞧࡞ࡓࡵ,ᆅẆࡢ඲㠃࡟ᆒ୍࡞ᅽຊࢆຍ࠼࡚ࡶ, ࡑࡢྛ㒊࡟࠾ࡅࡿṍࡳࡣ୍ᵝ࡛ࡣ࡞࠸ࡀ, ≉࡟ᆅẆࡢ୍ᒁ㒊ࢆ᤬ࡾ, ࠶ࡿ࠸ࡣ᭤ࡆࡿࡼ࠺࡞ṍࡳࢆ㉳ࡇࡍࡢࡣ, ࡴࡋࢁẼᅽ ࡢ໙㓄ࡢᙳ㡪ࡀ኱ࡁ࠸࡜ᛮࢃࢀࡿ. ࡇࡢ⪃࠼࡟ᇶ࡙ࡁ, ᪥ᮏྛᆅࡢẚ㍑ⓗ⊃࠸༊ᇦ 5 ࠿ᡤ࡟㝈ࡾ, ᆅ㟈ࡢศᕸ࡜Ẽᅽࡢ໙㓄࡜ࡢ㛫࡟ఱ➼࠿ࡢ㛵ಀࡀ࡞࠸࠿ㄪ࡭ࡓ. ⤖ᯝࡣ, ୧⪅ࡢ㛫࡟ఱ➼࠿ࡢᐦ᥋࡞㛵ಀࡀ࠶ࡿࡇ࡜ࢆ᝿ീࡉࡏࡿ࡟㊊ࡿࡇ࡜ࡀㄆࡵࡽࢀࡓࠒ(ᑎ⏣㸸ࠕᆅ㟈ࡢ㢖ᗘ࡜Ẽᅽࡢ໙㓄࡜ࡢ㛵ಀ࡟ᑵ࡚ࠖ.ࠗẼ㇟㞟ㄅ࠘.
28 ᖺ 1 ྕ. 1909. p.1ࠥ11㸭ㄽᩥ no. 㑥 2).
Dï2.

㛗ᒸ༙ኴ㑻ࡣ, ᑎ⏣ࡢࡇࡢㄽᩥࢆ࠺ࡅ࡚, ⌮ㄽⓗ⪃ᐹࢆ⾜ࡗࡓ( H. Nagaoka㸸Problem of Surface

Loading with Applications to Geophysical Phenomena. 3URFHHGLQJVRIWKH7RN\R0DWKHPDWLFRï3K\VLFDO

Society. Ser.ϩ, Vol. 6. 1912. 3. p. 208ࠥ215). ᮌᮧᮾసࡣ, ࡇࢀࢆḟࡢࡼ࠺࡟ゎㄝࡋ࡚࠸ࡿ. ࠕ(㛗ᒸࡣ)୍⯡ᘧ࠿ࡽࡣࡌࡵ࡚, ௒ᗘࡣ⾲㠃Ⲵ㔜࡟ࡼࡗ࡚⏕ࡎࡿ⾲㠃ࡢഴࡁࢆㄽࡌࡿ. ࡑࡋ࡚, ᅽຊ໙㓄ࡢᴟ኱Ⅼ௜
㏆࡟ᙎᛶࡢ◚ቯⅬࡀぢฟࡉࢀࡿࡇ࡜ࢆᣦ᦬ࡍࡿ. ࡲࡓ, ᭱኱ࡢഴᩳゅࢆࡶࡗࡓሙᡤࡣᅽຊ໙㓄ࡢᴟ኱Ⅼ௜㏆࡟࠶ࡾ, ࡇࢀࡣᑎ⏣ࡢ◊✲࡟୍⮴ࡍࡿ࡜࠸࠺ࠖ(ᮌᮧ㸸ࠗ㛗ᒸ༙ኴ㑻ఏ࠘. ᮅ᪥᪂⪺♫. 1973.

p. 367).

Dï3. ⛉Ꮫྐ◊✲⪅ࡢἩ ḟ㑻ࡣ,ࠕ኱᳃ᡣྜྷࡣ͐ ᆅ㟈Ⓨ⏕࡜Ẽᅽ࡜ࡢ㛵ಀࢆㄪ࡭, Ẽᅽࡀ㧗࠸࡜ࡁ࡟ᆅ㟈ࡀከࡃ㉳ࡁࡿഴྥࡀぢࡽࢀࡿ, ࡜ࡢㄽᩥࢆ࠸ࡃࡘࡶ᭩࠸ࡓ. ࡇࢀ࡟ᑐࡋ࡚ᑎ⏣ࡣ, Ẽᅽࡢ኱ᑠࡼࡾࡶẼᅽࡢ໙㓄ࡢ኱ᑠࡢ᪉ࡀᆅ㟈Ⓨ⏕࡟ᙳ㡪ࢆ୚࠼ࡿࡢ࡛ࡣ࡞࠸࠿࡜⪃࠼, ୰ኸẼ㇟ྎࡀࡲ࡜ࡵࡓẼᅽศᕸ࡜኱᳃࠿ࡽᥦ౪ࡉࢀࡓᆅ㟈ࢹ࣮ࢱࢆẚ㍑◊✲ࡋࡓ. ࡋ࠿ࡋ࡞ࡀࡽ, ࡇࡢㄽᩥ࡛ࡣ᫂☜࡞⤖ㄽࡣᚓࡽࢀ࡚࠸࡞࠸ࠖ࡜㏙࡭ࡓ (Ἡ㸸ࠗ᪥ᮏࡢᆅ㟈ண▱◊✲ 130 ᖺྐ࠘. ᮾி኱Ꮫฟ∧఍. 2015. p. 160).

‫ڦ‬6. ᪥ᮏࡢపẼᅽᛶ㝆㞵ࡢศᕸ.
A. The Distribution of Cyclonic Precipitation in Japan. Nature. Vol. 97, No. 2444. 1916. 8. 31. p.
550.
B. T. Terada, T. Yokota and S. Otuki㸸On the Distribution of Cyclonic Precipitation in Japan.

Journal of the College of Science, Tokyo Imperial University, Vol. 37, Art. 4, 1916. 1. p. 1ࠥ32. 㹙ㄽᩥ no. 55㹛.
C. ࠕThe paper is partly a statistical investigation of the influence of land and water in modifying therainfall from 1905 to 1915, but contains also an attempt to analyse the factors that determine the
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D.

³³³.

‫ڦ‬7. ᆅ☢Ẽࡢ⬦ື.
A. Terrestrial Magnetic Oscillations. Nature. Vol. 101, No. 2534. 1918. 5. 23. p. 233. By C. Chree.
B. T. Terada㸸On Rapid Periodic Variations of Terrestrial Magnetism. Part I and ϫ. Journal of theCollege of Science, Imperial University of Tokyo, Vol. 37, Art. 9. 1917. 5. p. 1ࠥ23, 23ࠥ47, 47ࠥ85 .
㹙ㄽᩥ no. 58ࠥ60㹛.
C.

ࠕThe paper referred to below is an important contribution to our knowledge of oscillations in the

PDJQHWLFHOHPHQWVHVSHFLDOO\WKRVHRIVKRUWHUSHULRGWHUPHG´SXOVDWLRQVµE\YDQ%HPPHOHQ« ࠖ.

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Dï1.

Ọ⏣ Ṋࡣࡇࡢ◊✲ࡢព⩏࡟ࡘࡁ, ḟࡢࡼ࠺࡟㏙࡭࡚࠸ࡿ.ࠕᆅ⌫☢ሙࡢ᪥࿘ኚ໬ࡸኴ㝜᫬ኚ໬ࡢ⤌⧊ⓗ◊✲ࡣ, ୺࡜ࡋ࡚ⱥᅜ࡟࠾࠸࡚௒ୡ⣖ࡢึࡵ࡟⾜ࢃࢀࡓ͐ ࢃࡀᅜ࡟࠾ࡅࡿࡇࡢ᪉㠃ࡢ᭱ึࡢࡲ࡜ࡲࡗࡓㄽᩥ࡜ࡋ࡚ᑎ⏣ᐥᙪඛ⏕ࡢ ´2Q5DSLG3HULRGLF9DULDWLRQVRI7HUUHVWULDO0DJQHWLVPµ ࡣ, ᙜ᫬ࡢᆅ☢Ẽ⬦ືࡢㄽᩥ࡜ࡋ࡚᏶⎍࡟㏆࠸ෆᐜ࡜ゝ࠼ࡿ࡛࠶ࢁ࠺. ͐ (ㄽᩥ୰ࡢ) ᩘ⌮ⓗ㆟ㄽࡢ㒊ศࡣ⌧ᅾࡢᆅ⌫ෆ㒊㟁☢ឤᛂㄽ࠿ࡽࡳ࡚ࡶṇࡋ࠸ෆᐜ࡛࠶ࡿࠖ(Ọ⏣㸸ࠕᆅ⌫☢ẼᏛ 100 ᖺࡢṌࡳࠖ.ࠗ⮬↛࠘. 29 ༹ 8 ྕ. 1974. 8.
p. 28ࠥ46).
Dï2.

␊ᒣஂᑦࡣㄒࡿ. ࠕࡇࢀࡣ୕ᓮἜናࡢὝ❍ࡢ୰࡛ᚓࡓᆅ☢Ẽ୕せ⣲ࡢ☢Ẽグ㘓ࢆᩚ⌮ࡋ࡚ฟࡉࢀࡓ⤖ᯝ࡛࠶ࡿ. ͐ ᕳ㢌࡟ࡣࠑᅾ⫋஧༑஬ᖺࢆ⚃ࡋ࡚⏣୰㤋ឡᶲᩍᤵ࡟ᤝࡆࡿࠒ࡜༳ๅࡋ࡚࠶ࡿ. ࡇࡢᆅ☢Ẽ⬦ືほࡢࡇ࡜ࡣ, ⏣୰㤋ඛ⏕ࡢᥦၐ࡛, 㟈⅏ண㜵ㄪᰝ఍ࡢ௙஦࡜ࡋ࡚, ᆅ㟈࡜ᆅ☢Ẽኚືࡢ㛵ಀࢆぢࡘࡅࡓ࠸࡜࠸࠺ࡇ࡜࡛ጞࡲࡗࡓࡶࡢ࡛࠶ࡿ͐ ⤖ㄽࢆゝ࠺࡜, ᆅ☢Ẽኚື࡜ᆅ㟈ࡢ㛵ಀࡣ࡞࠸ࡀᆅ☢Ẽ⬦ືࡢ࠸ࢁ࠸ࢁࡢᛶ㉁ࢆవࡍᡤ࡞ࡃゎᯒࡉࢀ, ᩘ⌮ⓗ࡟ᆅẆࡢ㟁☢ឤᛂࢆᢅࡗ࡚, ᐇ⤖ᯝ࡜ẚ㍑ࡍࡿࡇ࡜ࢆࡸࡗ

࡚࠾ࡽࢀࡿࡢ࡛࠶ࡿࠖ (␊ᒣ㸸ࠕⅆ⅏ㄽ, 㞾ࡑࡋ࡚ᆅ☢Ẽ⬦ືࠖ.Ᏹ⏣㐨㝯⦅ࠗ⛉Ꮫ⪅ ᑎ⏣ᐥᙪ࠘ࠑNHK ࣈࢵ
ࢡࢫ࣭225ࠒ. ᪥ᮏᨺ㏦ฟ∧༠఍. 1975. p. 91ࠥ109).

‫ڦ‬8. Ẽᅽࡢ᪥ኚ໬.
A. Diurnal Variation of Atmospheric Pressure. Nature. Vol. 101, No. 2535. 1918. 5. 30. p. 253ࠥ
254. By W. W. B.
B. T. Terada, M. Kiuti and Z. Tukamoto㸸On Diurnal Variation of Barometric Pressure. Journal ofthe College of Science, Tokyo Imperial University, Vol. 41, Art. 1. 1917. 11. p. 1ࠥ30. 㹙ㄽᩥ no. 62㹛.
C.

Nature ࡢグ஦ࡣ, ࠑDiurnal Variation of Atmospheric Pressureࠒ ࡢࢱ࢖ࢺࣝࡢࡶ࡜, ᑎ⏣ࡽࡢ࡯࠿,」ᩘࡢ◊✲⪅ࡢ◊✲ࢆࡶྜࢃࡏ⤂௓ࡋ࡚࠸ࡿ. 㛵ಀ㒊ศࢆᘬࡃ. ࠕThree Japanese investigators from theGeophysical Seminary of the Physical Institute, Tokyo, contribute an account of a preliminary attempt
to trace more detinitely the mechanism of these local influences , one of the most obvious of which ,XQGHUWKHQDPHRI´FRQWLQHQWDOLW\µKDs recent been attracting the attention of Mr. C. E. P. Brooks in thisFRXQWU\LQFRQQHFWLRQZLWKFOLPDWHDQGZLWKDSXUHO\JHRJUDSKLFDOWKHRU\RIWKH,FHDJH« ࠖ.
D.

³³³.

‫ڦ‬9. ᪥ᮏࡢ㝆㞵࡟ཬࡰࡍᆅᙧࡢᙳ㡪.
A. Effect of Topography on Precipitation in Japan. Nature. Vol. 105, No. 2645. 1920. 7. 8. p. 599
ࠥ600. By W. W. B.
B. T. Terada, M. Isimoto and M. Imamura㸸On the Effect of Topography on the Precipitation inJapan. Journal of the College of Science, Tokyo Imperial University, Vol. 41, Art. 5. 1919. 6. p. 1ࠥ
23.㹙ㄽᩥ no. 68㹛.
C.

Nature ࡢグ஦ࡣ, ࠑEffect of Topography on Precipitation in Japanࠒ ࡢࢱ࢖ࢺࣝࡢࡶ࡜, ᑎ⏣ࡽࡢ ࡯࠿, 」ᩘࡢ◊✲⪅ࡢ◊✲ࢆࡶྜࢃࡏ⤂௓ࡋ࡚࠸ࡿ. 㛵ಀ㒊ศࢆᘬࡃ. ࠕ$W ILUVW VLJKW 3URI 7HUDGD·V
contribution in the Journal of the College of Science, Tokyo Imperial University (vol. xli., art. 5), appears
to be only a supplement to previous work of Profs. Nakamura and Fujiwhara, but one or two
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parallelism than of cause and effect, for he prefers to attribute both phenomena to barometric changes
UDWKHUWKDQWRDVVRFLDWHWKHLQVWDELOLW\RIWKHVRLOZLWKSHUFRODWLRQ« ࠖ.
Dï1.

ࡇࡢㄽᩥ࡟ࡘࡁᑎ⏣⮬ࡽࡀゎㄝࡋ࡚࠸ࡿࡢ࡛ᘬࡃ. ࠕᆅ㟈ࡢ㢖ᗘ࡜Ẽ㇟⌧㇟࡜ࡢ㛫࡟Ꮡᅾࡍࡿࡽࡋ࠸㛵ಀ㹙࡟ࡘ࠸࡚㹛ᑎ⏣༤ኈࡣ, ᡃࡀᅜ࡟᪊ࡅࡿ㝆Ỉ㔞ࡢᆅ⌮ⓗศᕸ࡟㛵ࡍࡿ◊✲࠿ࡽࡋ࡚, ୰㒊᪥ᮏ࡟᪊ࡅࡿ୍⯡ࡢẼᅽࡢഴᗘࡀ, ᆅ㟈ࡢ㢖ᗘ࡜඼ࡢᆅ᪉ࡢ㝆Ỉ㔞࡜ࢆ஧ࡘஆࡽᐃࡵࡿࡶࡢ࡛࠶ࡽ࠺࡜⪃࡬ࡽࢀ࡚ᒃࡿࠖ(ᑎ⏣ᐥᙪ࣭ᯇ⃝Ṋ㞝ཎⴭ㸭ᆤ஭ᛅ஧ヂ⿵㸸ࠕᡃࡀᅜ࡟᪊ࡅࡿᆅ㟈ᏛࡢⓎ㐩ࠖ. ≀⌮Ꮫ㍯ㅮ఍ྠே⦅ࠗ≀⌮Ꮫᩥ⊩ᢒ࠘. ➨ 2 ㍴.
Dï2.

ᒾἼ᭩ᗑ.

1928. p. 19ࠥ20).

Ἡ ḟ㑻ࡢᮏ㸸ࠕᑎ⏣ࡣ, ᪥ᮏᾏഃ࡜ኴᖹὒഃࡢẼᅽࡢᕪࡀ኱ࡁ࠸ᖺ࡟ࡣ, Ⓨ⏕ࡋࡓᆅ㟈ࡢᩘࡀከ࠸ഴྥࡀぢࡽࢀࡿ࡜ࡢㄽᩥࢆ᭩࠸࡚࠸ࡿࠖ(Ἡ㸸ࠗ᪥ᮏࡢᆅ㟈ண▱◊✲ 130 ᖺྐ࠘. ᮾி኱Ꮫฟ∧఍. 2015.

p.

160).

‫ڦ‬10. ኴ㝧ࡢάື࡜ᆅ☢Ẽ.
A. Sunspot Frequencies and Terrestrial Phenomena³An Interesting paper . Nature. Vol. 119,No. 2990. 1927. 2. 19. p. 293.
B.

T. Terada㸸 On Some Remarkable Relation between the Yearly Variations of Terrestrial

phenomena and Solar Activities.

Journal of the College of Science, Tokyo Imperial University, Vol.

44, Art. 6. 1923. 1. p. 1ࠥ20.㹙ㄽᩥ no. 77㹛.
C.

Nature ࡢグ஦ࡣ,ࠑOur Astronomical Columnࠒḍࡢ」ᩘࡢグ஦ࡢ 1 ⦅࡜ࡋ࡚⤂௓ࡉࢀ࡚࠸ࡿ. 㛵ಀ㒊ศࢆ 1 㒊ᢒฟࡍࡿ.ࠕThe association of earthquakes with spot frequencies in the north and south
hemispheres of the sun, called Nand S,

is examined, and Terada finds that for some places in Japanand Jamaica, minima of earthquake frequency occur in years when N ï Sis small, while for others,

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D.

ᑎ⏣⮬ࡽࡢゎㄝࢆᘬࡃ. ࠕ㏆㡭, ᑎ⏣༤ኈࡢ◊✲࡟ࡼࡿ࡜, ᡈᆅ᪉ࡢẼᅽࡢᖺࠎࡢኚ໬࡜, ኴ㝧ࡢᩬග㹙㯮Ⅼ㹛ࡢศᕸࢆ♧ࡍᅉᩘ࡜ࡢ㛫ࡢ┦㛵㛵ಀࢆㄪ࡭࡚ࡳࡿ࡜, ᆅ᪉࡟ࡼࡗ࡚኱య஧ࡘࡢ✀㢮ࡀ࠶ࡗ࡚, ࠾஫࡟㏫ࡢᛶ㉁ࢆ♧ࡍᆅᇦ࡟ศࢀࡿ࡜࠸ࡩ஦࡛࠶ࡿ. ඼ୖ, Ṉࡢ஧✀㢮ࡢᆅ᪉ࡢศᕸࡀ, ୖ࡟㏙࡭ࡓᆅ㟈࡟ࡘ࠸࡚ࡢ஧✀㢮ࡢᆅ᪉ࡢศᕸ࡜, 㠀ᖖ࡟ࡼࡃఝ࡚࠸ࡿ࡜பࡩ஦࡛࠶ࡿࠖ(ᑎ⏣ᐥᙪ࣭ᯇ⃝Ṋ㞝 ཎⴭ㸭ᆤ஭ᛅ஧ヂ⿵㸸ࠕᡃࡀᅜ࡟᪊ࡅࡿᆅ㟈ᏛࡢⓎ㐩ࠖ. ≀⌮Ꮫ㍯ㅮ఍ྠே⦅ ࠗ≀⌮Ꮫᩥ⊩ᢒ࠘. ➨ 2 ㍴.
p. 12).

 

ᒾἼ᭩ᗑ.

1928.

‫ڦ‬11. ὶయࡢ㐠ື.
A. Fluid Vortices. Nature. Vol. 120, No. 3030. 1927. 11. 26. p. 784.
B. T. Terada and K. Hattori㸸Some Experiments on Motion of Fluids. Part I, ϩ and Ϫ. Reportsof the Aeronautical Research Institue, Tokyo Imperial University. Vol. 2. No. 16. 1926. 5. p. 85ࠥ
112.㹙ㄽᩥ no. 83㹛.
C. ࠕWith the object of supplying data for a more complete mathematical treatment of the vortices
formed in a fluid about a body rotating in it, or if this should prove impossible , for a qualitative
treatment of the problem. Messrs. T. Terada and K. Hattori, of the Aeronautical Research Institute of
the University of Tokyo, have made a photographic study of the forms of these vortices under variousERXQGDU\FRQGLWLRQV« ࠖ.
D.

ᑎ⏣㛛ୗࡢ⋢㔝ග⏨ࡣࡇࡢㄽᩥࢆヲࡋࡃゎㄝࡋ࡚࠸ࡿࡢ࡛ᢒฟࡍࡿ.ࠕ➨ 1 㒊࡟ሗ࿌ࡉࢀࡓᐇ㦂ࡣ, ኱ṇ 11 ᖺ 6 ᭶୰㡭࠿ࡽጞࡵࡽࢀࡓࡶࡢ࡛, ᙜ᫬✺Ⓨࡋࡓ⯟✵⯪ࡢ⇿Ⓨ஦௳ࡢཎᅉㄪᰝࡢ௙஦࡟㛵ಀࢆᣢࡓࢀ࡚࠸ࡓඛ⏕ࡣ, Ẽ⌫࠿ࡽ₃ࢀ࡛ࡿỈ⣲ࡢᣑࡀࡾ᪉࡞࡝ࢆㄪ࡭ࡿ┠ⓗ࡛⾜ࢃࢀࡓࡶࡢ࡛࠶ࡗࡓ. ᐇ㦂ࡣ࢞ࣛࢫᙇࡾࡢ⟽ࡢ୰࡟Ỉࢆ‶ࡓࡋ, ࡑࡢᗏ࡟࠾࠸ࡓ⣲↝ࡢ⟶࠿ࡽⰍࡢࡘ࠸ࡓ㍍࠸ᾮయࢆⁱࡳࡔࡉࡏ, ࡑࡢᾮࡀỈࡢ୰ࢆ❧ࡕ᪼ࡗ࡚⾜ࡃᶍᵝࢆ෗┿࡟࡜ࡗ࡚ࡋࡽ࡭ࡓ. ͐ ࡇࡢᐇ㦂࡟ࡼࡾ, ₃ࢀ࡛ࡓ㍍࠸ᾮయࡣ, Ỉࡢ୰ࢆ༢࡞ࡿᣑᩓࡢἲ๎࡟ࡼࡗ࡚ᣑࡀࡿࡢ࡛࡞ࡃ, ₃ฟࡢ㝿⏕ࡎࡿࡢస⏝ࢆ⪃៖ࡋ࡞ࡅࢀࡤ࡞ࡽ࡞࠸ࡇ࡜ࡀᣦ᦬ࡉࢀࡓ. ͐ ➨ 2 㒊࡛ࡣ, ᑐὶ࡟ࡼࡿᾮయ㐠ືࡢ◊✲ᐇ㦂ࢆ㏙࡭࡚࠸ࡿ. 㛗᪉ᙧࡢ࢞ࣛࢫᙇࡾᐜჾࡢ୰
࡟Ỉࢆධࢀ, ᐜჾࡢᗏࡢ࠸ࢁ࠸ࢁࡢሙᡤ࡟࠾࠿ࢀࡓ㟁⇕ᯈ࡟ࡼࡗ࡚࡝ࢇ࡞ὶయ㐠ືࡀ࠾ࡇࡿ࠿ࢆㄪ࡭ࡓ.
Ỉࡢ㐠ື≧ែࢆ▱ࡿࡓࡵ࡟, Ỉࡢ୰࡟⣽࠿࠸࢔࣑ࣝࢽ࣒࢘ࡢ⢊ᮎࢆᩓࡽࡋ, ࡇࢀ࡟㐺ᙜ࡞↷᫂ࢆࡋ࡚ከᩘࡢ෗┿ࢆ࡜ࡗ࡚㐠ືࡢᶍᵝࢆㄪ࡭ࡓ. ࡇࡢࡼ࠺࡞ሙྜࡢỈࡢ㐠ືࡣ, ᬑ㏻࡟⪃࠼ࡽࢀࡿࡼ࠺࡞⡆༢࡞ᐃᖖⓗ࡞ᚠ⎔ὶ࡛ࡣ࡞ࡃ, ᗄࡘ࠿ࡢࡲ࡜ࡲࡗࡓᕳࡀ࡛ࡁ, ࡑࢀࡽࡢᕳࡢศᕸࡸ┦஫స⏝࡟ࡼࡗ࡚ᴟࡵ࡚」㞧࡞ὶࡀ⏕ࡎࡿ. ࡇࡢ」㞧࡞㐠ືࢆ㏻ほࡋ࡚͐ ୍⯡ⓗ࡞⪃࠼᪉࡟㐩ࡋࡓ. ➨ 3 㒊࡛ࡣ, ඛ⏕ࡀ኱ṇ 12 ᖺࡢ㛵ᮾ኱ᆅ㟈ࡢ㝿, ᮾி࡟⏕ࡌࡓ኱᪕㢼࡟ࡘ࠸࡚, 㟈⅏ண㜵ㄪᰝ఍ࡢ௙஦࡟㛵㐃ࡋ࡚, ≉࡟㛵ᚰࢆࡶࡓࢀࡓ
❳ᕳࡢ⏕ᡂ࡟㛵ࡍࡿᐇ㦂ⓗ◊✲ࡢ୍㒊ࡀ㏙࡭ࡽࢀ࡚࠶ࡿࠖ(⋢㔝㸸ࠕᑎ⏣ඛ⏕࡜⦅ࠗ⛉Ꮫ⪅ ᑎ⏣ᐥᙪ࠘ࠑNHK ࣈࢵࢡࢫ࣭225ࠒ.᪥ᮏᨺ㏦ฟ∧༠఍.

࡟㛵ࡍࡿ◊✲ࠖ.Ᏹ⏣㐨㝯

1975. p. 151ࠥ172).

‫ڦ‬12. 㟁Ẽⅆⰼ.
A. Electric Sparks. Nature. Vol. 122, No. 3063. 1928. 7. 14. p. 73ࠥ74.
B. T. Terada and U. Nakaya㸸Experimental Studies on Form and Structure of Sparks. Part I,ϩand Ϫ. Scientific Papers of the Institute of Physical and Chemical Research , Tokyo, Vol. 8,No.

131. 1928. 2. p. 1ࠥ19㸹Vol. 8, No. 135. 1928. 2. p. 63ࠥ82㸹 Vol. 8, No. 138. 1928. 3. p. 103ࠥ129.
㹙ㄽᩥ no. 99, 101, 109㹛.
C.

ࠕThe three experimental papers on the form and structure of electric sparks, by T. Terada and U.

Nakaya, published in volume 8 of the Scientific Papers of the Institute of Physical and Chemical Research, Tokyo, are instructive to scientific workers and will be useful to magneto manufacturers. Theauthors point out that our present knowledge of the form and structure of sparks is not much greater
WKDQLQWKHGD\VRI)UDQNOLQDQG/LFKWHQEHUJ«D.

ࠖ.

୰㇂Ᏹྜྷ㑻ࡀ, ୍⣔ࡢࡇࡢ◊✲ࡢព⩏ࢆゎㄝࡋ࡚࠸ࡿࡢ࡛ᘬࡃ. ࠕ1 Ẽᅽࡢ✵Ẽ୰ࡢⅆⰼࡣ, 㟁ᴟ㛫ࡢ㊥㞳ࡀ▷࠸㛫ࡣ┤⥺࡛᭱▷㊥㞳ࢆ㣕ࡪࡀ, ᑡࡋ㛗ࡃ࡞ࡿ࡜ᬑ㏻ࡣ✄ጔᙧ࡜ࡶ⛠ࡍ࡭ࡁᢡࢀ᭤ࡗࡓᙧࢆ࡜ࡿ஦ࡣ, ࿘▱ࡢ஦ᐇ࡛࠶ࡿ. ͐ Ṉ➼ࡢ⡆༢࡞↛ࡋஆࡽⅆⰼ࡟㛵ࡍࡿ┤᥋ࡢᛶ㉁࡟㛵ࡍࡿ◊✲ࡣ, ᚑ᮶Ṥࢇ࡝㛩༷ࡉࢀ࡚ᒃ࡚, 㦫ࡃ࡭ࡁከᩘࡢᩥ⊩ࡣṤࢇ࡝పᅽࡢᡤㅝ ┿✵ᨺ㟁, ཪࡣ 1 Ẽᅽ୰࡛ࡣᴟࡃ▷࠸ⅆⰼ࡟ᑵ࠸࡚, ඼ࡢⅆⰼ㟁ᅽ, ⅆⰼࡢ㐜ࢀ➼ࡢ ͆ᩘ್ࢆᐃ͇ ࡍࡿ஦࡟㝈ࡽࢀ࡚ᒃࡿ. ᩘ್ࡢᐃ࡟ࡣ෌⌧ྍ⬟୍࡛␒⡆༢࡞᮲௳ࢆ㑅ࡪᚲせࡀ࠶ࡿ, ࡑࢀ࡛୙つ๎࡞ᙧࢆ࡜ࡿ㛗࠸ⅆⰼࡣ, ෌⌧୙⬟࡜ࡋ࡚◊✲ࡢᑐ㇟࡟ࡉࢀ࡞࠸ഴࡀ࠶ࡗࡓ. ↛ࡋ௨ୗ࡟㏙࡭ࡿᵝ࡟ⅆⰼࡢᆺࢆศ㢮ࡋ, ࡑࡢᡂ❧ࡢ᮲௳ࢆ⢭ࡋࡃㄪ࡭ࡿ࡜, ྛࠎࡢᆺ࡟ࡘ࠸࡚ࡣ෌⌧ࡀྍ⬟࡛࠶ࡾ, ྠ୍ᆺ࡟ᒓࡍࡿಶࠎࡢⅆⰼ࡟ᑵ࠸࡚ࡣ, ⤫ィⓗἲ๎ࡢᡂ❧ࡢྍ⬟ᛶࡀ࠶ࡿ஦ࡀศࡗࡓࠖ(୰㇂㸸ࠗẼయෆ㟁Ẽ⌧㇟࠘ࠑᒾἼㅮᗙ ≀⌮Ꮫཬࡧ໬Ꮫ. ≀⌮Ꮫ. Ϯ. Bࠒ. 1931. ࠕ§29. 㟁Ẽⅆⰼࡢᙧཬࡧᵓ㐀ࡢ◊✲ࠖ. p. 61ࠥ66).

‫ڦ‬ᮏከ࣭ᑎ⏣ࡽࡢㄽᩥ The Secondary Oscillation of Ocean Tides ࡢ⤂௓グ஦[ᩥ⊩ No. 2㹛㸬 