NASA216 頁
組員任務後彙報
NASA不明飛行物體D015太空人科學任務歸詢 1962年 1963年
日期範圍15 NOVEMBER 1963
出處/單位NASA
NASA 檔案系列中的組員任務後彙報,共 216 頁。文件中提及日期:15 NOVEMBER 1963、21 FEBRUARY 1962、24 MAY 1962。下方節錄與重點均自原檔文字層直接抽取。
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NASA 釋出的載人月球或軌道任務語音/彙報紀錄。
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- p.5EN· C 11.gbt. tll&t ,, C COIie t I bo • • at boti. ,tbeil l ltlQ'ecl 1n 1 j( tbe ~ ont.bento • Dee'中文· C 11.gbt. tll&t ,, C COIie t I bo • • at boti. ,tbeil l ltlQ'ecl 1n 1 j( tbe ~ ont.bento • Dee'
- p.15EN· 4中文· 4
- p.32EN· ~--...........--......................,..__. t中文· ~--...........--......................,..__. t
- p.34EN· From t.l¼e~-eie Vconsiderations alone, it may be stated that the luminous Jparticles observed by Col中文· From t.l¼e~-eie Vconsiderations alone, it may be stated that the luminous Jparticles observed by Col
- p.35EN· The fact that the coloring a,~aPen~ ~~~,~ was a yellow-green and the eiiee~ive observational pi,e became fluorescent in sunlight.~e particles observed in shadow were observed in the scattered light from the spacecraft and were probably illuminated only by visible ~ ~~f the spectrum. - ;l- The change of angles of t…· Glenn to observe the particles under improper dark adaptation ~ indicate'that an astronaut would be in a position to carry through a series of experi'1nents to investigate C.o~.L" the physics of Q.QmROMS in the solar environment中文· The fact that the coloring a,~aPen~ ~~~,~ was a yellow-green and the eiiee~ive observational pi,e became fluorescent in sunlight.~e particles observed in shadow were observed in the scattered light from the spacecraft and were probably illuminated only by visible ~ ~~f the spectrum. - ;l- The change of angles of t…· Glenn to observe the particles under improper dark adaptation ~ indicate'that an astronaut would be in a position to carry through a series of experi'1nents to investigate C.o~.L" the physics of Q.QmROMS in the solar environment
- p.36EN· Glenn's observation -.'t o{ '- band six to eight degrees 9'f t~e twill a-eix-~e-eiga~-aegPee-e&Ba above the horizon, with a haze layer about two degrees Although it has been speculated that wide at the top. ~5'~~1!:irl~-.eilli-il~e observation = ~\: the multipa~wl:l:,ers of the1'window cause the high 0~ angle~ the …· Au-6her investigations of the air glow and haze layerKiG£ should be carried out . ~~ Meteorology中文· Glenn's observation -.'t o{ '- band six to eight degrees 9'f t~e twill a-eix-~e-eiga~-aegPee-e&Ba above the horizon, with a haze layer about two degrees Although it has been speculated that wide at the top. ~5'~~1!:irl~-.eilli-il~e observation = ~\: the multipa~wl:l:,ers of the1'window cause the high 0~ angle~ the …· Au-6her investigations of the air glow and haze layerKiG£ should be carried out . ~~ Meteorology
- p.37EN· It is of se.e:~ a:t-importanli" that proper dark adaptation methods be incorporated into the spacecraft system so that the astronaut may optimize his visual observations. c o"'tl'le\.s Investigations of the physics of OQB!!fteft~s and the feasibility of the ~l " th-tificial ~omet "experiment may be carried out direc…中文· It is of se.e:~ a:t-importanli" that proper dark adaptation methods be incorporated into the spacecraft system so that the astronaut may optimize his visual observations. c o"'tl'le\.s Investigations of the physics of OQB!!fteft~s and the feasibility of the ~l " th-tificial ~omet "experiment may be carried out direc…
- p.38EN· A..~,:...... >MC,--. p .,..c,,h ...~ o... multi lier :Be! "b systeml ~ series of filters r: 4,-~J ►"'-> --~c.~... ~-- .t..~--~ ~ u.v. ~\_,..,, - ...~ (including~a J;,Oii~e flaorceeent ~lain fi]:l;er to stuely ½ ~t-..Av,.u.,,,-.o:..c.. ) tac ultra viole:!T) should be incorporated into the spacecraft. ~iUJ£e -a :au.m…中文· A..~,:...... >MC,--. p .,..c,,h ...~ o... multi lier :Be! "b systeml ~ series of filters r: 4,-~J ►"'-> --~c.~... ~-- .t..~--~ ~ u.v. ~\_,..,, - ...~ (including~a J;,Oii~e flaorceeent ~lain fi]:l;er to stuely ½ ~t-..Av,.u.,,,-.o:..c.. ) tac ultra viole:!T) should be incorporated into the spacecraft. ~iUJ£e -a :au.m…
- p.39EN· B 2 3 196? 0 U.\h <!.°""""U)4.. '2'"3ol!I- '3oco 0 ~ -~ Vje0/2 w~Jo...:, caJ v-nf c~-4中文· B 2 3 196? 0 U.\h <!.°""""U)4.. '2'"3ol!I- '3oco 0 ~ -~ Vje0/2 w~Jo...:, caJ v-nf c~-4
- p.40EN· It seemed possible that the layer he described could be . accounted for as a region of relatively large nitrogen peroxide (N02 ) concentration, and the past two weeks have been spent in checking this hypothesis • Unfortunately I am not familiar with either photochemistry or upper atmosphere physics so the following …中文· It seemed possible that the layer he described could be . accounted for as a region of relatively large nitrogen peroxide (N02 ) concentration, and the past two weeks have been spent in checking this hypothesis • Unfortunately I am not familiar with either photochemistry or upper atmosphere physics so the following …
- p.41EN· Figure 1 I Vertical path (No. 1) No. 3 No. 2 Figure 2中文· Figure 1 I Vertical path (No. 1) No. 3 No. 2 Figure 2
- p.42EN· Ju}¥ 13, 1962 Fox- th, followins I will assume that the concentr.ation ot absorbins mo1ecu1es in the region of interest can be described adequate}¥ by an exponential decrease w1th altitude above the bottom, of the layer, hence, can be represented by where Y is the scale height in the layer and H must lie in the .ia.yer中文· Ju}¥ 13, 1962 Fox- th, followins I will assume that the concentr.ation ot absorbins mo1ecu1es in the region of interest can be described adequate}¥ by an exponential decrease w1th altitude above the bottom, of the layer, hence, can be represented by where Y is the scale height in the layer and H must lie in the .ia.yer