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electrojet £Û£é£ì¢¥£å£ë£ô£ò¡Ó£ä¬Ù£à£å£ô£Ý °íÃþÀü·ù(»óÃþ ´ë±âÀÇ ÀÌ¿ÂÀÇ È帧)

F layer 1Ãþ(Áö»ó 200, 300km »óÃþÀÇ Àü¸®Ãþ, ´ÜÆÄ¸¦ ¹Ý»ç)

merolect £Û£í¢¥£å£ó¡Ó£ì£å£ë£ô£Ý ÁßÃþ ¹æ¾ð(»óÃþ ¹æ¾ð°ú, ÇÏÃþ ¹Ù¾ðÀÇ Áß°£¿¡ ÀÖ´Â ¾ð¾î º¯Á¾)

neve £Û£î£å£é£ö¢¥£å£é£Ý ¸¸³â¼³(ºùÇÏÀÇ »óÃþºÎ¸¦ Çü¼ºÇÏ´Â ÀÔ»ó ºù¼³

radiometeorograph £Û£ò£à£å£é£ä£é£ï£õ£í£é:£ô£é¢¥£ï:£ò¡Ó£ç£ò£à©¡£æ£Ý ´ë±â »óÃþÀÇ ±â»ó °üÃø ÀåÄ¡(radi osonde)

radiosonde £Û£ò¢¥£å£é£ä£é£ï£õ£ó£à£á£î£ä£Ý ¶óµð¿À Á¸µ¥(radiometeorograph)(´ë±â »óÃþÀÇ ±â»ó »óŸ¦ ÃøÁ¤ÇÏ¿© ÀüÆÄ·Î Áö»ó¿¡ ¼Û½ÅÇÏ´Â ±â°è)

rawinsonde £Û£ò¢¥£å£é£÷£é£î£ó£à£á£î£ä£Ý ·¹ÀÌÀ©Á¸µ¥(»óÃþdz °üÃø¿ë ¶óµð¿À Á¸µ¥)

stratocruiser £Û£ó£ô£ò¢¥©¡£ô£ï£õ£ë£ò£à£õ:£ú¡Ó£ò£Ý »óÃþ±Ç ºñÇà±â

superstratum £Û£ó¢¥£õ:£ð¡Ó£ò£ó£ô£ò£å£é£ô¡Ó£í£Ý »óÃþ

topper £Û£ô£à£á£ð¡Ó£ò£Ý À§(»óÃþ)ÀǰÍ, (°úÀÏ µûÀ§) Àß º¸ÀÌ·Á°í À§¿¡ ¾ñÀº ÁÁÀº °Í, ¿ì¼öÇÑ »ç¶÷(°Í), ¶Ù¾î³­ °Í

topsider £Û£ô¢¥£á£ð£ó£à£á£é£ä¡Ó£ò£Ý (Á¶Á÷ÀÇ)»óÃþºÎ, ¼ö³úºÎ(ÀÇ »ç¶÷), »ó°©ÆÇ ½Â¹«¿ø(´ã´ç Àå±³)

topper ¿©¼º¿ë °¡º­¿î ¿ÜÅõ, »óµîǰ, ¿ì·®Ç°, »óÃþÀÇ °Í

[±×¸®½º½ÅÈ­] ¡¼¿¹Å׸£(aether)¡½ ½ÅÀûÀÎ ÈûÀ¸·Î µ¤¿©ÀÖ´Â ´ë±âÀÇ »óÃþºÎ³ª ½ÅÀ»
µÑ·¯½Î°í ÀÖ´Â °ø±â. ¶ÇÇÑ Æ¯È÷ û¸íÇÑ ÇÏ´ÃÀ» ¶æÇϱ⵵ Çß´Ù.

[ÛÝ] »óÃþ±â´Ü (ß¾öµÑ¨Ó¥) superior air mass

[ÛÝ] »óÃþ¿î (ß¾öµê£) high level clouds

[ÛÝ] »óÃþ¹Ù¶÷ upper wind

[ÛÝ] »óÃþ¿ªÀüÃþ (ß¾öµæ½ï®öµ) upper layer inversion

[ÛÝ] »óÃþ¾ð¾î (ß¾öµåëåÞ) superstratum

acrolect »óÃþ¹æ¾ð

Some continental rocks are over 3,000 million years old, while those of
the ocean floor are less then 200 million years old. The crusts and the
top, solid part of the mantle, totaling about 70 to 100 kilometers in
thickness, at present appear to consist of about 15 rigid plates, 7 of
which are very large. These plates move over the semimolten lower mantle
to produce all of the major topographical features of the Earth. Active
zones where intense deformation occurs are confined to the narrow,
interconnecting boundaries of contact of the plates.
¾î¶² ´ë·úÀÇ ¹ÙÀ§´Â 30¾ï ³â ÀÌ»ó µÇ¾ú°í ¹Ý¸é¿¡ ¹Ù´Ù¹Ù´ÚÀÇ ¹ÙÀ§µéÀº 2¾ï ³â
ÀÌÇÏÀÇ ³ªÀÌÀÌ´Ù. ´Ù ÇÕÃļ­ µÎ²²·Î ¾à 70 ³»Áö 100 km µÇ´Â, Áö°¢°ú ¸ÇƲÀÇ
´Ü´ÜÇÏ°í °¡º­¿î »óÃþºÎ´Â ÇöÀç ¾à 15°³ÀÇ ´Ü´ÜÇÑ ÁöÆÇÀ¸·Î ±¸¼ºµÇ´Â °ÍÀ¸·Î
º¸À̴µ¥, ±× ÁßÀÇ 7 °³´Â ¸Å¿ì Å« °ÍµéÀÌ´Ù. ÀÌ ÁöÆÇµéÀº ¹ÝÂë ³ì¾ÆÀÖ´Â
ÇÏÃþºÎ ¸ÇƲÀÇ À§·Î ¿òÁ÷¿© ´Ù´Ï¸é¼­ Áö±¸ÀÇ ¸ðµç ÁÖ¿äÇÑ ÁöÇüÀûÀΠƯÁúµéÀ»
»ý¼ºÇس½´Ù. °­·ÂÇÑ º¯ÇüÀÌ ¹ß»ýÇϴ Ȱµ¿ÀûÀÎ Áö¿ªÀº, Á¼À¸¸é¼­ »óÈ£°áÇÕµÈ
ÁöÆÇµéÀÇ Á¢ÃË °æ°è¼±ºÎºÐ¿¡ ±¹ÇѵȴÙ.

As we descend into the darkness, the pressure builds, the temperature falls.
¾ÏÈæ¼¼°è·Î ³»·Á°¨¿¡ µû¶ó ¾Ð·ÂÀº ³ô¾ÆÁö°í, ¿Âµµ´Â ³»·Á°©´Ï´Ù
Below five hundred meters, new, mysterious animals appear.
500¹ÌÅÍ ¾Æ·¡·Î ³»·Á°¡¸é »õ·Ó°í ½ÅºñÇÑ µ¿¹°ÀÌ ³ªÅ¸³³´Ï´Ù
Their bizarre shapes help them to remain suspended in the dark space.
ÀÌó·³ ±«»óÇÑ ¸ð½ÀÀÌ µÈ °ÍÀº ¾îµÒ¼Ó¿¡¼­ ¶°ÀÖ±â ÆíÇϱ⠶§¹®ÀÔ´Ï´Ù
Some resemble creatures familiar from shallower waters
ÀϺΠ¾ÔÀº ¹Ù´Ù »ý¹°°ú ´àÀº »ý¹°µµ ÀÖÁö¸¸
others defy classification.
¹ÌºÐ·ùÁ¾µµ ¸¹½À´Ï´Ù
All around, organic particles drift downwards.
¿Â »ç¹æ¿¡´Â À¯±â¹°ÀÌ ¾Æ·¡·Î ¶³¾îÁö°í ÀÖ½À´Ï´Ù
Marine snow, detritus from the creatures swarming in the sunlit waters above.
¹Ù´Ù´«Àº ÇÞºûÀÌ µå´Â »óÃþºÎ »ý¹°ÀÇ Â±âÀÔ´Ï´Ù
The snow is food for many animals here, like the sea spider
¹Ù´Ù´«Àº ¹Ù´Ù°Å¹Ì¸¦ ºñ·ÔÇÑ À̰÷ µ¿¹°ÀÇ ¸ÔÀÌÀÔ´Ï´Ù
a small relative of shrimps and crabs.
¹Ù´Ù°Å¹Ì´Â »õ¿ì³ª °ÔÀÇ Ä£Ã´»¹ÀÎ ¼ÒÇü»ý¹°ÀÔ´Ï´Ù
Those strange leg-like appendages are feathered, to stop it from sinking.
ÀÌ»óÇÑ ´Ù¸®¸ð¾çÀÇ ºÎ¼Ó±â°ü¿£ ÅÐÀÌ ´Þ·ÁÀÖ¾î °¡¶ó¾ÉÁö ¾Ê½À´Ï´Ù
They can also enmesh marine snow
¹Ù´Ù´« äÁý¿¡µµ À¯¿ëÇÏÁÒ
which it wipes carefully into it's jaws.
Á¶½É½º·´°Ô °É·¯³»¾î ÀÔÀ¸·Î °¡Á®°©´Ï´Ù

superior air mass »óÃþ ±â´Ü

upper winds »óÃþ ¹Ù¶÷

decantation : °æ»çºÐ¸®, »óÃþ¾×ºÐ¸®, ±â¿ï¿© µû¸£±â

decanter : °æ»çºÐ¸®±â, »óÃþ¾×ºÐ¸®±â

upper cloud : »óÃþ¿î

»óÃþ ´ë±â upper atmosphere

»óÃþ Àü¸®Ãþ °üÃø topside sounding

pull of the superior retrodiscal lamina (¿øÆÇ ÈÄÁ¶Á÷ »óÃþÀÇ °ßÀÎ)

superior retrodiscal lamina (¿øÆÇÈÄÁ¶Á÷ »óÃþ) ¿øÆÇÈÄÁ¶Á÷À̳ª ÈÄ¹æ ºÎÂøºÎÀÇ ÃÖ»ó¹æ ¸é.

top (»óÃþ)

[ùþ]high cloud »óÃþ¿î

(100)½Ç¸®ÄÜ ±âÆÇÀÇ °áÁ¤¹æÇâ¿¡ µû¸¥ ´Ù°øÁú ½Ç¸®ÄÜ Çü¼ºÀÇ À̹漺¿¡ °üÇÑ ¿¬±¸
Anisotropic Property of Porous Silicon Formation Dependent on Crystal
Direction of (100) Silicon Substrates
-
´Ù°øÁú ½Ç¸®ÄÜÀ» Çü¼ºÇϴµ¥ À־ À̹漺 ¾ç±Ø ¹ÝÀÀ °úÁ¤À» °üÂûÇÏ¿´´Ù.
We have observed anisotropic anodisation process for porous silicon formation.
½ÇÇèÀç·á´Â nÇü ±âÆÇÀ§¿¡ n+°¡ È®»êµÇ°í ±× À§¿¡ n ¿¡ÇÇÃþÀÌ ÀÖ´Â
n/n+/n ±¸Á¶ÀÇ (100) ½Ç¸®ÄÜ ¿þÀÌÆÛ¿´´Ù.
The starting material was (100) silicon n/n+/n wafer structured by
n+ -diffusion on n-type substrate and by subsequent n-epitaxial growth.
»óÃþºÎ n ½Ç¸®ÄÜ ¿¡ÇÇÃþÀ» ½Ä°¢ÇÏ¿© ´Ù°øÁú ½Ç¸®ÄÜ ÃþÀÇ ¾ç±Ø ¹ÝÀÀ âÀ» ³»°í
¾ç±Ø¹ÝÀÀÀÌ n+¸Å¸ôÃþ±îÁö¸¸ ÀϾ°Ô ÇÑ´Ù.
After the top n-silicon epitaxial layer was etched to open the porous
silicon layer(PSL) anodisation window, anodisation takes place only
to n+ -buried layer.
´Ù°øÁú ½Ç¸®ÄÜ ÃþÀÇ Çü¼º°úÁ¤Àº À̹漺À̾ú´Ù.
The process of porous silicon formation on (100) sample was anisotropic,
¹ÝÀÀâÀÇ ÇüŵéÀÌ ¼­·Î ´Ù¸¦Áö¶óµµ ¹ÝÀÀµÈ ´Ù°øÁú ½Ç¸®ÄÜ ¿µ¿ªÀÇ
¸ð¾çÀº ¸ðµÎ »ç°¢Çü ÇüÅÂÀÇ °ÍÀ̾ú´Ù.
which was evident from that the shapes of the reacted porous silicon layer
was all squarelike regardless of the shapes of reaction windows.
ÀÌ ½ÇÇè °á°ú´Â ´Ù°øÁú ½Ç¸®ÄÜ ¾ç±Ø¹ÝÀÀÀº È­ÇйÝÀÀ¿¡ ´Þ·Á ÀÖ´Â °ÍÀÌ ¾Æ´Ï°í
Àü±âÀüµµ ¼ºÁú Áï °áÁ¤¹æÇâ¿¡ µû¸¥ Á¤°øÀÇ ¼­·Î ´Ù¸¥ Àüµµµµ¿¡ ÀÖ´Ù´Â °ÍÀ» º¸¿©ÁØ´Ù.
The experimental results show that the PSL anodisation process
does not depend on chemical reaction but does on electrical conduction property,
which is hole mobility depending on the crystal direction.

Krasnopolsky said the proven abundance of water in Mars¡¯ early
history ¡°improves the prospects¡± that life could have evolved there.
In a study appearing Friday in the journal Science, planetary
researchers Krasnopolsky and Paul D. Feldman of Johns Hopkins
University said that Mars¡¯ upper atmosphere contains molecular
hydrogen, or H2, a finding that confirms earlier theoretical
models of the water history of the planet.
Å©¶ó½º³ëÆú½ºÅ°´Â È­¼º Ãʱ⿡ ¹°ÀÌ ¸¹ÀÌ ÀÖ¾ú´Ù´Â °ÍÀÌ Áõ¸íµÈ
°ÍÀº È­¼º¿¡¼­ »ý¸íü°¡ ÁøÈ­ÇßÀ» ¼öµµ ÀÖ´Ù´Â ¡°°¡´É¼ºÀ» ÁøÀü½ÃŰ´Â
°Í¡±À̶ó°í ¸»Çß´Ù.
¡®»çÀ̾𽺡¯Áö ±Ý¿äÀÏÀÚ¿¡ ½Ç¸° Ç༺ÇÐÀÚµéÀÎ Å©¶ó½º³ëÆú½ºÅ°¿Í
Á¸½ºÈ©Å²½º´ëÇÐ Æú D. Æçµå¸ÕÀº È­¼ºÀÇ »óÃþ ´ë±â¿¡ ¼ö¼ÒºÐÀÚ (H2)°¡
Æ÷ÇԵŠÀÖ°í ÀÌ´Â È­¼º¿¡ ¹°ÀÌ Á¸ÀçÇß´ø ½Ã´ë¿¡ ´ëÇÑ ÀÌ·ÐÀû ¸ðµ¨À»
ÀÔÁõÇÏ´Â °ÍÀ̶ó°í ¹àÇû´Ù.

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