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ºùÇϱâ HOME > ÀÚ·á½Ç > ºùÇϱâ
ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 12Àå
ºùÇÙÀº ¼ö¸¸ ³âÀ» º¸¿©Áִ°¡?
(Frozen in Time, Chapter 12.
Do Ice Cores Show Many Tens of Thousands of Years?)
Michael J. Oard

    ºùÇÏÇÐÀÚµéÀº ±×¸°¶õµå ºù»óÀÇ À§¿¡¼­ºÎÅÍ ¾Æ·¡·Î ¿¬·ûÃþ(annual layer)À» ¼¼¾î¼­ ³ªÀÌ(¿¬´ë)¸¦ °è»êÇÒ ¼ö ÀÖ´Ù°í ÁÖÀåÇÑ´Ù. ±×µéÀº ºù»óÀÇ »óÀ§ 90%¸¦ ¼¼¾î¼­ 110,000³âÀ» ÃßÁ¤Çϰí ÀÖ´Ù. ±×µéÀÇ ÁÖÀåÀº Á¤´çÇѰ¡?

â¼¼±â ´ëÈ«¼ö¿¡ ÀÇÇØ ¿øÀÎµÈ ºùÇϱ⠸ðµ¨ÀÇ »ç°Ç ¼ø¼­¿¡ µû¸£¸é, ÇØºù±â ¸»¿¡ ºùÇϱⰡ »ç½Ç»ó Á¾·áµÇ¾ú´Ù. ÇÏÁö¸¸ ÀϺΠºù»óÀº °è¼ÓÇØ¼­ ÀÚ¶ó³µ´Ù. ±×¸°¶õµå¿Í ³²±Ø´ë·ú¿¡ ÀÖ´Â ºù»óÀº â¼¼±â ´ëÈ«¼ö¿¡ ÀÇÇÑ ºùÇϱâ ÀÌÈÄÀÇ ÀÜÁ¸¹°ÀÌ´Ù(±×¸² 12.1, 12.2). ±× ºù»óµéÀº ±ØÁö¹æ¿¡ À§Ä¡ÇØÀÖ¾ú°í, ºùÇϱ⵿¾È ³ôÀº °íµµ¿¡ ÀÖ´ø ¾óÀ½À̾ú±â ¶§¹®¿¡, ¿ëÀ¶À¸·ÎºÎÅÍ º¸Á¸µÆ´Ù. ´ë±â´Â °íµµ°¡ 1,000m ³ô¾ÆÁú¼ö·Ï Æò±Õ 6¡ÆC°¡ ³·¾ÆÁö±â ¶§¹®¿¡, ¾óÀ½ÀÇ °íµµ´Â ÇϳªÀÇ Áß¿äÇÑ ¿ä¼ÒÀÌ´Ù.

ºùÇϱ⠸»¿¡ ±×¸°¶õµå¿Í ³²±Ø´ë·úÀÇ Ãʱ⠾óÀ½ÀÇ µÎ²²°¡ µÎ²®Áö ¾Ê¾Ò´Ù¸é, ±×°÷ÀÇ ºù»óÀº ÇöÀç Å©±â·Î ÀÚ¶óÁö ¾Ê¾ÒÀ» ¼öµµ ÀÖ´Ù´Â °ÍÀº Èï¹Ì·Ó´Ù. ¾î¶² °úÇÐÀÚµéÀº ¾î¶»°Ôµç ¾óÀ½ÀÌ »ç¶óÁ³´Ù¸é, ÇöÀçÀÇ ±âÈÄ¿¡¼­´Â ºùÇϰ¡ ´Ù½Ã »ý°Ü³ªÁö ¾Ê¾ÒÀ» °ÍÀ̶ó°í ¹Ï°í ÀÖ´Ù. À̰ÍÀº ƯÈ÷ ±×¸°¶õµåÀÇ °æ¿ì¿¡ ±×·¯ÇÏ´Ù.

1960³â´ë ÀÌÈÄ ³²±Ø´ë·ú ºù»ó°ú ±×¸°¶õµå ºù»ó¿¡ ´ëÇÑ ¸¹Àº ±¼ÂøµéÀÌ ÀÖ¾ú°í ±íÀº °÷ÀÇ ºùÇÙ(ice cores)µéÀÌ Ã¤ÃëµÇ¾ú´Ù.(±×¸² 12.1, 12.2¸¦ º¸¶ó). ¿À´Ã³¯ ºù»óµéÀº °èÀý¿¡ µû¶ó ¼øÈ¯ÇÏ´Â ¸ÕÁö, »ê¼º¹°Áú, ¿À¿°¹°Áú µîÀ» Æ÷ÇÔÇϰí ÀÖ´Ù. ºù»óÀÇ »ó´Ü ºÎ±Ù¿¡¼­´Â °èÀý°ú °ü·ÃµÈ ¸¹Àº º¯¼öµéÀ» ÃøÁ¤ÇÔÀ¸·Î½á, ¿¬·ûÃþÀ» ±¸ºÐÇÒ ¼ö ÀÖ´Ù. ºùÇÏÇÐÀÚµéÀº ±×¸°¶õµå ºù»óÀÇ ²À´ë±â¿¡¼­ ¾Æ·¡·Î ³»·Á°¡¸é¼­ ¿¬·ûÃþ(annual layers)µéÀ» ¼¼¾î¼­, ³ª¹«ÀÇ ³ªÀÌÅ׸¦ ¼¼µíÀÌ ¿¬´ë(³ªÀÌ)¸¦ °è»êÇÒ ¼ö ÀÖ´Ù°í ÁÖÀåÇÑ´Ù. ±×µéÀº ºù»óÀÇ »óÀ§ 90%¸¦ ¼¼¾î¼­ 110,000³âÀ» ÃßÁ¤Çϰí ÀÖ´Ù.[1] ±×µéÀÇ ÁÖÀåÀº Á¤´çÇѰ¡?

 

 

 

 

 

 

 

 

 

 

 

±×¸² 12.1. ÁÖ¿ä ºùÇÙµéÀÇ À§Ä¡¿Í ÇØ¼ö¸é À§ÀÇ ¾óÀ½ µÎ²²¸¦ º¸¿©ÁÖ´Â ±×¸°¶õµåÀÇ Áöµµ.(Redrawn by Ron Hight).

 

 

 

 

 

 

 

 

 

 

 

 

 

±×¸² 12.2. ÁÖ¿ä ºùÇÙµéÀÇ À§Ä¡¿Í ÇØ¼ö¸é À§ÀÇ ¾óÀ½ µÎ²²¸¦ º¸¿©ÁÖ´Â ³²±ØÀÇ Áöµµ.(Redrawn by Ron Hight).


±×¸°¶õµå ºù»ó¿¡´Â 11¸¸ °³ÀÇ ¿¬·ûÃþµéÀÌ Àִ°¡?

±×¸°¶õµå ºù»ó ¹Ø¹Ù´Ú ±Ùó±îÁöÀÇ GISP2 ºùÇÙ¿¡´Â 110,000°³ÀÇ ¿¬·ûÃþµéÀÌ ÀÖ´Ù°í ÁÖÀåµÇ°í Àִµ¥, À̰ÍÀº Á÷Á¢ÀûÀÎ ÃøÁ¤ÀÌ ¾Æ´Ï´Ù. ¿¬·ûÃþÀº ½ÇÁ¦·Î ºù»óÀÇ »ó´Ü ±Ùó¿¡´Â Àß ³ªÅ¸³­´Ù. ±×·¯³ª ºù»óÀÇ ¼ÓÀ¸·Î ±íÀÌ µé¾î°¥¼ö·Ï, »óȲÀº ÈξÀ ´õ º¹ÀâÇÏ´Ù. ±Ùº»ÀûÀ¸·Î µ¿ÀϰúÁ¤¼³À» ÁÖÀåÇÏ´Â °úÇÐÀÚµéÀº ¿¬·ûÃþÀ» °áÁ¤Çϱâ À§Çؼ­´Â ºù»óÀÇ ¹Ù´Ú°ú Áß°£ ºÎºÐ¿¡ ´ëÇÑ °¡Á¤(assumptions)µéÀ» ¼¼¿ö¾ß ÇÑ´Ù.

ÁÖ¿äÇÑ °¡Á¤Àº Áö±¸ÀÇ ³ªÀ̰¡ ¼ö½Ê¾ï ³â µÇ¾ú´Ù°í °¡Á¤ÇÏ´Â °ÍÀÌ´Ù. ±×µéÀº ±×¸°¶õµå ºù»ó°ú ³²±Ø ºù»óÀÌ À屸ÇÑ ½Ã°£ µ¿¾È Á¸ÀçÇØ¿Ô¾ú´Ù°í °¡Á¤ÇÑ´Ù. °Ô´Ù°¡, ±×µéÀº ÀÌ ºù»óÀÌ À屸ÇÑ ½Ã°£ µ¿¾È ÆòÇü»óÅ¿¡¼­ ÇöÀçÀÇ ³ôÀ̸¦ °ÅÀÇ À¯ÁöÇØ¿Ô´Ù°í ¹Ï´Â´Ù. ±×µéÀº ÇØ¸¶´Ù ºù»êÀÌ ³ì°í ¶³¾îÁ®³ª°¡ ÀÒ¾î¹ö¸° ¾óÀ½°ú, ¸Å³â ´õÇØÁö´Â ´«°ú ¾óÀ½ÀÇ ¾çÀÌ Àý¹¦ÇÏ°Ô ±ÕÇüÀ» ÀÌ·ç¾î¿Ô¾ú´Ù°í »ý°¢ÇÑ´Ù. ±×µéÀÇ ÀÌ·¯ÇÑ °¡Á¤ ¶§¹®¿¡, µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº ¿¬·ûÃþÀº ´õ ¸¹Àº ´«°ú ¾óÀ½À¸·Î µ¤¿©Áö±â ¶§¹®¿¡, ±ØÀûÀ¸·Î ¾ã¾ÆÁ³À» °ÍÀ̶ó°í ¹Ï´Â´Ù(±×¸² 12.3). ±×µéÀÇ °¡Á¤¿¡ ÀÇÇÑ °á·ÐÀº, ¿¬·ûÃþÀÇ ¾ÐÃà Á¤µµ´Â ¾óÀ½ÀÌ ¾ó¸¶³ª ¿À·¡µÈ °ÍÀÎÁö¿¡ ´Þ·ÁÀÖ´Ù´Â °ÍÀÌ´Ù. ¼ö¹é¸¸ ³â µ¿¾È ÆòÇü»óÅ¿¡ ÀÖ¾î¿Ô´ø ºù»ó¿¡¼­, ¿¬·ûÃþÀº ÀÌ·ÐÀûÀ¸·Î ±Þ°ÝÈ÷ ¾ã¾ÆÁ®¼­, ºùÇÏÀÇ ¹Ù´Ú ±Ùó¿¡¼­´Â °ÅÀÇ Á¾ÀÌó·³ ¾ã¾ÆÁ³À» °ÍÀ̶ó°í »ý°¢ÇÑ´Ù.

 

 

 

 

 

 

±×¸² 12.3. ºùÇÏÀÇ ¿¬·ûÃþÀº ¼öÁ÷ÀûÀ¸·Î ¾ÐÃàµÇ°í, À§·Î ´©ÀûµÇ´Â ´«°ú ¾óÀ½ÀÇ ¾Ð·ÂÀ¸·Î ÀÎÇØ¼­ ¼öÆòÀûÀ¸·Î ´Ã¾î³­´Ù.

´Ù¸¥ ÇÑÆíÀ¸·Î, â¼¼±â ´ëÈ«¼ö¿¡ ÀÇÇØ ¿øÀÎµÈ ºùÇϱ⠸𵨿¡¼­¿Í °°ÀÌ ¾óÀ½ ÃþÀÌ ºü¸£°Ô Çü¼ºµÇ¾ú´Ù¸é, ¿¬·ûÃþÀº ¹Ù´Ú¿¡¼­ ¸Å¿ì µÎ²®°í, À§·Î °¥¼ö·Ï ¾ã¾ÆÁ®¼­, ÇöÀçÀÇ ¿¬·ûÃþ µÎ²²°¡ µÇ¾úÀ» °ÍÀÌ´Ù. ¹°·Ð ÀÌ ÂªÀº ±â°£ µ¿¾È¿¡µµ ¾óÀ½¿¡ ¾à°£ÀÇ ¾ÐÃàÀº ÀÖ¾úÀ» °ÍÀÌ´Ù. ±×·¯³ª ±×°ÍÀº µ¿ÀϰúÁ¤¼³ ¸ðµ¨ÀÌ Á¦½ÃÇÏ´Â °Íº¸´Ù ÈξÀ Àû¾úÀ» °ÍÀÌ´Ù.[2] ±×¸² 12.4´Â ±íÀÌ¿¡ µû¸¥ ¿¬·ûÃþ µÎ²²¿¡ ´ëÇÑ ÀÌ·¯ÇÑ ´ëÁ¶ÀûÀÎ °ßÇØ¸¦ º¸¿©ÁØ´Ù.

 

 

 

 

 

 

 

 

 

±×¸² 12.4 µ¿ÀϰúÁ¤¼³ ¸ðµ¨[4] ¹× âÁ¶·Ð ¸ðµ¨[5]¿¡ µû¶ó °è»êµÈ, ±×¸°¶õµå ÁߺΠGRIP ºùÇÙÀÇ ¿¬·ûÃþ µÎ²².

°¡Á¤µÇ´Â ¿¬·ûÃþÀÇ µÎ²²´Â ÃøÁ¤µÈ ¿¬·ûÃþÀÇ µÎ²²¸¦ ÇØ¼®ÇÏ´Â µ¥¿¡ ±âÃʰ¡ µÇ±â ¶§¹®¿¡ Áß¿äÇÏ´Ù. ÃøÁ¤Ä¡´Â ¿¬·ûÃþÀÇ °¡Á¤µÈ µÎ²²¿¡¼­ ¾à°£ ¹þ¾î³¯ ¼ö´Â ÀÖÁö¸¸, ¸¹ÀÌ ¹þ¾î³ªÁö´Â ¾Ê´Â´Ù. ¿¹¸¦ µé¾î, »ê¼Òµ¿À§¿ø¼Ò ÃøÁ¤¹ý(oxygen isotope method)¿¡¼­ µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº º¸Åë '¿¬°£¡± Ç¥Áö¸¦ ¾ò±â À§Çؼ­´Â ¿¬·û Áֱ⠴ç 8°³ÀÇ ÃøÁ¤À» ÇÊ¿ä·Î ÇÑ´Ù. ¿¹¸¦ µé¾î, µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº ´ë·« 1,600m(1¸¶ÀÏ) ±íÀÌÀÇ GRIP ±×¸°¶õµå ºùÇÙÀÇ Áß°£ ºÎ±Ù¿¡¼­ ¿¬·ûÃþ µÎ²²°¡ 10cm¶ó°í ¹Ï°í ÀÖ´Ù.[3]. ±×·¸´Ù¸é »ê¼Òµ¿À§¿ø¼Ò ÃøÁ¤Àº ¸Å 1cm °£°Ý ¸¶´Ù ½Ç½ÃÇØ¾ß ÇÑ´Ù.

âÁ¶·Ð ¸ðµ¨Àº ¿¬·ûÃþ µÎ²²°¡ 30cm Á¤µµ·Î ÈξÀ µÎ²®´Ù°í °¡Á¤Çϰí Àֱ⠶§¹®¿¡, µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº ÇÊ¿ä ÀÌ»óÀ¸·Î ´õ ¸¹Àº ÃøÁ¤µéÀ» Çß°í, µû¶ó¼­ 1³â ³»ÀÇ ¿©·¯ »ê¼Òµ¿À§¿ø¼Ò ÁÖ±âµéÀ» ÃøÁ¤Çß´ø °ÍÀÌ´Ù. ÀÌ°Í ¶§¹®¿¡ ¿¬·ûÃþÀÇ ¼ö°¡ Å©°Ô °úÀåµÇ°Ô µÇ¾ú´Ù.[6]

ÀÌ¹Ì ¾ð±ÞÇßµíÀÌ, ±×¸°¶õµå ºù»óÀÇ »óºÎ¿¡ ´ëÇÑ ¿¬·ûÃþ µÎ²² ÃßÁ¤Ä¡´Â µ¿ÀϰúÁ¤¼³ °úÇÐÀÚ¿Í Ã¢Á¶·ÐÀÚÀÇ °á°ú°¡ °ÅÀÇ µ¿ÀÏÇÏ´Ù. µÎ ¸ðµ¨ÀÇ Â÷ÀÌ´Â ºùÇÙÀÇ ¾Æ·¡ÂÊÀ¸·Î °¥¼ö·Ï ´õ Ä¿Áø´Ù. âÁ¶·Ð ¸ðµ¨¿¡ ºñÇØ¼­ µ¿ÀϰúÁ¤¼³ ¸ðµ¨Àº ºùÇÙÀÇ ¸Ç ¾Æ·¡¿¡¼­ ¿¬·ûÃþÀÌ ±Ø´ÜÀûÀ¸·Î ¾ã±â ¶§¹®¿¡, µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº 1³âÀ» ³ªÅ¸³½´Ù°í »ý°¢ÇÏ´Â Ãþµé 100°³¸¦ 100³âÀ¸·Î »ý°¢ÇÒ ¼ö ÀÖÁö¸¸, âÁ¶·Ð ¸ðµ¨¿¡ ÀÇÇϸé À̵é 100°³ÀÇ ¿¬·ûÃþµéÀº ´ÜÁö 1³âÀ» ³ªÅ¸³¾ ¼ö ÀÖ´Ù. µû¶ó¼­ µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀº ½ÇÁ¦·Î Á¾Á¾ 1³â µ¿¾È ¹Ýº¹ÇÏ¿© ÀϾ ¼ö ÀÖ¾ú´ø ´« ÆøÇ³µéÀÇ Ãþµé, ¶Ç´Â ´Ù¸¥ ÁÖ±âÀû ³¯¾¾¿¡ ÀÇÇØ »ý°Ü³­ ÃþµéÀ» ¼¼°í ÀÖ¾ú´ø °ÍÀÏ ¼ö ÀÖ´Ù.[7] ¿¹¸¦ µé¾î, ´« ÆøÇ³Àº º¯¼öÀÇ ÃøÁ¤À» ´Þ¸®ÇÔ¿¡ µû¶ó µû¶æÇÑ ºÎºÐ°ú Â÷°¡¿î ºÎºÐÀ» °®°í Àִµ¥, À̰ÍÀº ÀÌ·¯ÇÑ º¯¼ö¿¡ µû¸¥ Áֱ⸦ ¸¸µé¾î³½´Ù. ÀÌ·¯ÇÑ ´« ÆøÇ³ÀÇ Áøµ¿(oscillations)Àº ¼öÀÏ Á¤µµÀÇ Áֱ⸦ °¡Áú ¼ö ÀÖ´Ù. µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÁ¶Â÷µµ, ´« ÆøÇ³°ú À̵¿ÇÏ´Â ´« ¾ð´ö(snow dunes)µé°ú °°Àº ´Ù¸¥ Çö»óµéÀÌ 1³âÀ» ³ªÅ¸³¾ ¼öµµ ÀÖ´Ù´Â °ÍÀ» ÀÎÁ¤Çϰí ÀÖ´Ù. ¾Ù¸®(Alley)¿Í µ¿·áµéÀº[8] ´ÙÀ½°ú °°ÀÌ ¸»ÇÑ´Ù :

±âº»ÀûÀ¸·Î 1³âÀÇ ±â°£À» ³ªÅ¸³»´Â Ç¥Áö(marker)¸¦ ¼¿ ¶§, ¿ì¸®´Â ±×°ÍÀÌ Àý´ëÀûÀ¸·Î ¸í¹éÇÑÁö, ¶Ç´Â ºñ¿¬°£(1³â µ¿¾È¿¡ ¿©·¯ ¹ø ÀϾ´Â) »ç°ÇÀÌ 1³âó·³ º¸ÀÌ´ÂÁö ¿©ºÎ¸¦ µûÁ®ºÁ¾ß ÇÑ´Ù. ´«¿¡ º¸ÀÌ´Â Ãþµé(±×¸°¶õµå Á߽ɺθ¦ ´ëÇ¥ÇÏ´Â ÃàÀû·ü¿¡ ´ëÇÑ ´Ù¸¥ ¿¬°£ Ç¥Áö)ÀÇ °æ¿ì¿¡, °èÀý ³»ÀÇ º¯µ¿, ÆøÇ³ÀÇ Á¤µµ µî¿¡ µû¸¥ º¯µ¿ µîÀÌ ¿¬°£ ¼öÁØÀÇ º¯µ¿ ³»¿¡ Á¸ÀçÇÒ ¼ö ÀÖ´Ù. ¿ì¸®´Â È®½ÇÈ÷ Ä¿´Ù¶õ ´« ÆøÇ³À̳ª ´« ¾ð´öÀÇ ÅðÀû¹°µéÀ» 1³âÀ¸·Î ¿ÀÀÎÇϰųª, ¾àÇÑ ¿©¸§À» ³õÃļ­ 2³âÀÇ °£°ÝÀ» 1³âÀ¸·Î ¼±ÅÃÇßÀ» °¡´É¼ºÀ» °í·ÁÇØ¾ß ÇÑ´Ù.


±×µéÀº ³²±Ø ºù»ó¿¡¼­ 70¸¸ ³âÀ» ÃøÁ¤ÇßÀ»±î?

¿¬·ûÃþÀ» ¼¼´Â ¹æ¹ýÀº ¸¹Àº ´«ÀÌ ÃàÀûµÇ´Â ±×¸°¶õµå ºù»ó(Greenland ice sheet)¿¡¼­¸¸ ÀÛµ¿µÈ´Ù. ±×·¯³ª ±íÀº ³²±Ø ºù»ó(Antarctic ice sheet)ÀÇ ºùÇÙÀº 30¸¸ ³âÀÌ ³Ñ¾î, ¹Ýº¹µÈ ¿©·¯ ¹øÀÇ ºùÇϱâµéÀ» ³ªÅ¸³½´Ù°í ÇÑ´Ù. ³²±Ø ºù»óÀÇ ²À´ë±â¿¡¼­ ½Ç½ÃµÈ »õ·Î¿î ¡®µ¼ C ºùÇÙ(Dome C ice core)¡¯Àº ¹Ù´Ú ±Ùó±îÁö ÃÑ 70¸¸ ³â µ¿¾È 7¹øÀÇ ºùÇϱ⸦ ¶ÕÀº °ÍÀ¸·Î ÁÖÀåµÇ°í ÀÖ´Ù. ÀÌ ³ªÀÌ´Â °´°üÀûÀÎ °ÍÀϱî?

³²±Ø´ë·ú ºù»óÀº ´ÜÁö ÇÑ ¹øÀÇ ºùÇϱ⸦ ³ªÅ¸³»´Â ÇØ¾È°¡ ºùÇÙÀ» Á¦¿ÜÇϰí, ºùÇϱ⿡ ´ëÇÑ Ãµ¹®ÇÐÀû ÀÌ·Ð(¹Ð¶õÄÚºñÄ¡ ÀÌ·Ð)ÀÌ Á¤È®ÇÏ´Ù´Â °¡Á¤ ÇÏ¿¡ ÃßÁ¤µÈ ¿¬´ëÀÌ´Ù.[9] (ÃÖ±Ù ¹Ð¶õÄÚºñÄ¡ ÀÌ·ÐÀº ºÎÁ¤µÇ¾ú´Ù. ÀÚ¼¼ÇÑ ³»¿ëÀº ¿©±â¸¦ Ŭ¸¯). »ç½Ç ÀÌ °¡Á¤Àº ±×¸°¶õµå ºù»óÀÇ ¿¬·ûÃþ ¿¬´ëÀÇ ÃßÁ¤¿¡µµ ¶ÇÇÑ °­·ÂÇÑ ±Ù°Å°¡ µÆ¾ú´Ù.[10] ÀÌ °¡Á¤Àº ±×µéÀÌ °¢ ÁֱⰡ 10¸¸ ³âÀÌ µÇ´Â ¼¼ °³ ÀÌ»óÀÇ ºùÇϱâ Áֱ⸦ ¾ò°Ô µÆ´ø ¹æ¹ýÀÌ´Ù. ±×µéÀº ´Ü¼øÈ÷ °¡Á¤µÇ´Â ºùÇϱâ ÁÖ±âµéÀÇ ¼ýÀÚ¸¦ ¼¼°í, õ¹®ÇÐÀû À̷п¡ ÀÇÇØ °¡Á¤µÈ ±â°£ÀÎ 10¸¸ ³âÀ» °öÇÑ´Ù. ÀÌ·¯ÇÑ ¿¬´ë´Â °´°üÀûÀÌÁö ¾Ê´Ù. ±×µéÀº ´Ü¼øÈ÷ õ¹®ÇÐÀû À̷аú ¿À·¡µÈ ¿¬´ë¶ó´Â °¡Á¤¿¡ ±âÃÊÇϰí ÀÖ´Â °ÍÀÌ´Ù. À̰ÍÀº 6Àå¿¡¼­ ³íÀǵƾú´Ù. ¾Æ·¡¿¡¼­ º¼ ¼ö ÀÖµíÀÌ, âÁ¶·ÐÀÇ Æ² ¾È¿¡¼­ ºù»ó ¹× ºùÇÙ µ¥ÀÌÅ͵éÀ» ÀçÇØ¼®ÇÏ´Â °ÍÀº ½¬¿î ÀÏÀÌ´Ù.


±×¸°¶õµå ¹× ³²±Ø ºù»ó - ´ëÈ«¼ö ÀÌÈÄ ºùÇϱâÀÇ ÀÜÁ¸¹°

ºùÇϱâÀÇ ÀýÁ¤±â¿¡ ºÏ¹Ý±¸ ºù»óÀÇ Æò±Õ µÎ²²´Â 700mÀÎ ¹Ý¸é, ³²±Ø¿¡¼­´Â 1,200m Á¤µµ ¿´´ø °ÍÀ¸·Î ÃßÁ¤µÈ´Ù. ¹Ù´å¹°Àº ¿©ÀüÈ÷ Æò±Õ 10¡ÆC·Î ºñ±³Àû µû¶æÇß´Ù. ¿À´Ã³¯ÀÇ Æò±Õ ¿ÂµµÀÎ 4¡ÆC¿¡ µµ´ÞÇϱâ À§Çؼ­´Â ´Ù½Ã 6¡ÆC Á¤µµ°¡ ´õ ³Ã°¢µÆÀ» °ÍÀÌ´Ù. Åðºù±â µ¿¾È ±×¸°¶õµå¿Í ³²±Ø´ë·ú¿¡ ÀÎÁ¢ÇØÀÖ´ø »ó´ëÀûÀ¸·Î µû¶æÇÑ ¹Ù´å¹°Àº Áö¼ÓÀûÀ¸·Î ÈξÀ Å« ÇØ¾ç Áõ¹ßÀ» ÀÏÀ¸ÄÑ, »ó´ëÀûÀ¸·Î ¸¹Àº ·®ÀÇ ´«À» ±×¸°¶õµå ¹× ³²±Ø´ë·úÀÇ ºù»ó¿¡ ³»¸®°Ô ÇßÀ» °ÍÀÌ´Ù.

ºùÇϱâÀÇ ÀýÁ¤ ÀÌÈÄ¿¡µµ ¾óÀ½ÀÇ ¼ºÀå ¼Óµµ°¡ Áö¼ÓµÆ´Ù¸é, Åðºù±â 200³â µ¿¾È ¹Ù´Ù´Â ÇöÀçÀÇ ¿Âµµ·Î ³Ã°¢µÇ¸é¼­, 30% ÀÌ»óÀÇ ¾óÀ½ÀÌ ±×¸°¶õµå¿Í ³²±Ø´ë·ú¿¡ Ãß°¡µÇ¾úÀ» °ÍÀÌ´Ù. ÀÌ ±â°£ÀÌ ³¡³ª¸é¼­ ±×¸°¶õµåÀÇ Æò±Õ ºùÇÏ µÎ²²´Â ¾à 900m, ³²±ØÀÇ Æò±Õ ºùÇÏ µÎ²²´Â ¾à 1,500m°¡ µÇ¾úÀ» °ÍÀÌ´Ù. ¿À´Ã³¯ ±×¸°¶õµå ºù»óÀÇ Æò±Õ µÎ²²´Â 1,600mÀ̸ç, ÃÖ´ë µÎ²²´Â 3,367mÀÌ´Ù.[11] ³²±Ø´ë·ú ºù»óÀÇ ÇöÀç Æò±Õ µÎ²²´Â 1,900mÀ̸ç, ÃÖ´ë µÎ²²´Â ¾à 4,200mÀÌ´Ù.

±×¸°¶õµå ºù»ó¿¡¼­ °­¼³·®À» ¹°·Î ȯ»êÇÑ °­¼ö·®Àº 30cm/³âÀ̸ç, ³²µ¿ÂÊ ¸ð¼­¸® Áö¿ªÀº 150cm/³â ÀÌ»óÀ̰í, ºù»óÀÇ ºÏÂÊ ¹ÝÂÊÀÇ ÀϺΠÁö¿ªÀº 20cm/³â ¹Ì¸¸ÀÌ´Ù.[13] ³²±Ø´ë·úÀÇ Æò±Õ °­¼ö·®Àº 19cm/³âÀ̸ç, ÀÌ °ªÀº ÇØ¾È ±ÙóÀÇ »ó´ëÀûÀ¸·Î ³ôÀº °­¼ö·®°ú, ³²±Ø ºù»óÀÇ µ¿ÂÊ ³ôÀº Áö¿ªÀÇ ´ëºÎºÐ°ú´Â 5cm/³â±îÁö Â÷À̰¡ Å©´Ù.[14] ³²±Ø ºù»óÀÇ ³ôÀº °íµµ¿¡¼­´Â °­¼ö·®ÀÌ ¸Å¿ì ³·¾Æ, ÀÌ Áö¿ªÀÌ ±ØÁö »ç¸·À¸·Î ¿©°ÜÁö°í ÀÖ´Â °ÍÀº Èï¹Ì·Ó´Ù.

±×¸°¶õµå ºù»óÀÇ ³²µ¿ºÎ Áö¿ªÀº ³î¶ó¿ï Á¤µµ·Î °­¼³·®ÀÌ ¸¹´Ù. Á¦2Â÷ ¼¼°è´ëÀü ÁßÀÌ´ø 1942³â¿¡ P-38 ÀüÅõ±â 6´ë¿Í B-17 Æø°Ý±â 2´ë°¡ ¹Ù´Ù¿¡¼­ 29km ¶³¾îÁø ±×¸°¶õµå ³²µ¿ºÎ ºù»ó¿¡ ºÒ½ÃÂøÇß´Ù. 1980³â´ë ÈĹݿ¡ ÇÑ Å½»çÆÀÀÌ ºñÇà±âµéÀ» ã¾Æ ³ª¼¹°í, 1942³â ÀÌÈÄ ºñÇà±âµéÀÌ 75m ´«¾óÀ½ ¾Æ·¡¿¡ ¹¯ÇôÀÖ´Ù´Â »ç½ÇÀ» ¹ß°ßÇß´Ù![15] ÀÌ ºñÇà±âµéÀº ž纹»ç¿­À» Èí¼öÇØ¼­ ºù»ó ¼ÓÀ¸·Î °¡¶ó¾É¾Ò´ø °ÍÀÌ ¾Æ´Ï´Ù. ºñÇà±âµéÀº ±× Áö¿ªÀÇ ³ôÀº °­¼³·® ¶§¹®¿¡ ªÀº ±â°£ µ¿¾È¿¡µµ ±íÀº ´«¾óÀ½ ¾Æ·¡¿¡ ¹¯È÷°Ô µÆ´ø °ÍÀÌ´Ù.(¾Æ·¡ °ü·ÃÀڷḵũ 51, 52 ÂüÁ¶). ±×·¯ÇÑ ³ôÀº °­¼³·®ÀÌ ºù»óÀÇ ´Ù¸¥ ºÎºÐµé¿¡ ´ëÇØ¼­µµ °°Àº °ÍÀº ¾Æ´Ï°ÚÁö¸¸, ºùÇϱ⿡ ºù»óµéÀº ÈξÀ ³·Àº °íµµ·Î ÀÖ¾ú°í, ±âÈĵµ ¸Å¿ì ´Þ¶úÀ» °¡´É¼º¿¡ ´ëÇÑ ÈùÆ®¸¦ ÁØ´Ù.

 

 

 

 

 

 

 

±×¸² 12.5. ´ëÈ«¼ö°¡ ³¡³­ ÀÌÈĺÎÅÍ ÇöÀç±îÁöÀÇ ½Ã°£¿¡ µû¸¥ ±×¸°¶õµå ¹× ³²±Ø ºù»óÀÇ ÃàÀû.

¼º°æÀû ¿¬´ë±â°¡ Á¤È®Çϸç, Á·ÀåµéÀÇ ¸ñ·Ï¿¡ ºüÁø °÷ÀÌ ¾ø´Ù°í °¡Á¤ÇÒ ¶§, ºùÇϱâ´Â ¾à 4õ ³â Àü¿¡ ³¡³µ´Ù. ±× ÀÌÈÄ·Î, ±×¸°¶õµå¿Í ³²±Ø ºù»ó¿¡ ¼ö¹é ¹ÌÅÍÀÇ ¾óÀ½ÀÌ Ãß°¡µÇ¾úÀ» °ÍÀÌ´Ù. ¹°·Ð, ÀÌ ½Ã±â µ¿¾È¿¡ ¾óÀ½ÀÌ ¼Õ½ÇµÇ±âµµ ÇßÀ» °ÍÀÌ´Ù. ±×·¯ÇÑ ¼Õ½ÇÀº ÁÖ·Î ºùÇÏÀÇ Ç¥¸éÀÌ ³ì¾Æ¼­ »ý±â´Â °ÍÀε¥, À̰ÍÀº ºù»êÀÌ ³ì¾Æ¼­ ¶³¾îÁ®³ª°¡´Â ±×¸°¶õµå ºù»ó¿¡¼­¸¸ ¶Ñ·ÇÇÑ Çö»óÀÌ´Ù. ¾óÀ½ÀÌ ³ì°í ºù»êÀÌ ¶³¾îÁ®³ª°¨¿¡µµ ºÒ±¸Çϰí, ÀÌ µÎ ºù»óÀº ºùÇϱⰡ ³¡³­ ÈÄ ¾à 4,000³â µ¿¾È ÇöÀçÀÇ µÎ²²±îÁö °è¼Ó ½×¿´À» °¡´É¼ºÀÌ ¸Å¿ì ³ô´Ù.

ÀÌ Ã¥¿¡ Á¦½ÃµÈ ¸ðµ¨Àº ¾à 700³â°£ Áö¼ÓµÆ´ø ÇÑ ¹øÀÇ ÂªÀº ºùÇϱ⠵¿¾È, ±×¸°¶õµå ºù»ó°ú ³²±Ø´ë·ú ºù»óÀÇ »ó´ç ºÎºÐÀÌ Çü¼ºµÈ °Í°ú, ¶Ç ´Ù¸¥ 3,700³â µ¿¾È ÇöÀç ±âÈİ¡ À¯ÁöµÈ °ÍÀ» ¼³¸íÇÒ ¼ö ÀÖ´Ù.[16] ±×¸² 12.5´Â ´ëÈ«¼ö°¡ ³¡³­ ÀÌÈĺÎÅÍ ÇöÀç±îÁö ºù»óÀÇ ÃàÀûÀ» ½Ã°£ ¼ø¼­·Î º¸¿©ÁØ´Ù.


ºùÇϱ⠵¿¾ÈÀÇ ºùÇÙ¿¡ °üÇÑ ¾û¶×ÇÑ ÇØ¼®µé

±×¸°¶õµå ºù»ó¿¡¼­ äÃëÇÑ ºùÇÙÀÇ ¾Æ·¡ÂÊ ÇϹݺΠ¶Ç´Â ºùÇϱ⠺κÐÀÇ '¿¬·ûÃþ(annual layers)¡±µé¿¡ ´ëÇÑ µ¿ÀϰúÁ¤¼³Àû ÇØ¼®Àº ¾û¶×ÇÑ °³³äµéÀ» ÃÊ·¡Çß´Ù.[17] ºùÇÙÀÇ ÇϹݺο¡ ÀÖ´Â ÀϺΠº¯¼öµéÀº ±ØÀûÀ̰í, ±Þ°ÝÇÑ º¯È­¸¦ ³ªÅ¸³»°í ÀÖ´Ù.(±×¸² 12.6). µû¶ó¼­ ÁÖ·ù°úÇÐÀÚµéÀº ±×µéÀÇ µ¿ÀϰúÁ¤¼³Àû °¡Á¤¿¡ µû¶ó, ÀÌ»óÇÑ °á·Ð¿¡ µµ´ÞÇÏ°Ô µÇ¾ú´Ù. ±×µéÀº ºùÇϱ⠳»¿¡¼­ ÀÌ·¯ÇÑ º¯µ¿À» ±×¸°¶õµåÀÇ ¿Âµµ°¡ ¼ö½Ê ³âÀ̶ó´Â ªÀº ±â°£ ¸¸¿¡ ÃÖ´ë 20¡ÆC±îÁö º¯È­µÆ´ø °ÍÀ¸·Î ÇØ¼®Çϰí ÀÖ¾ú´Ù![18]

±×¸² 12.6. ºùÇϱ⠵¿¾È ±â¿Â¿¡ ºñ·ÊÇÒ °ÍÀ¸·Î ÃßÁ¤ÇÏ´Â GISP2 ºùÇÙ »ê¼Òµ¿À§¿ø¼Ò º¯µ¿ÀÇ ±×·¡ÇÁ(M. Schultz) [19]

ÀÌ·¯ÇÑ º¯µ¿Àº Á÷Àü °£ºù±â¸¦ ³ªÅ¸³¾ °ÍÀ¸·Î »ý°¢µÇ´Â ºùÇÙÀÇ ¸Ç ¾Æ·¡±îÁö °è¼ÓµÈ´Ù. ÀϺΠ°úÇÐÀÚµéÀº ÀÌ º¯µ¿ÀÌ °£ºù±â µ¿¾ÈÀÇ ±Þ°ÝÇÑ ¿Âµµ º¯È­¶ó°í »ý°¢Çϰí ÀÖ´Ù. ¿ì¸®´Â °£ºù±â·Î ÃßÁ¤µÇ´Â ±â°£¿¡ »ì°í Àֱ⠶§¹®¿¡, ±×·¯ÇÑ ±ÞÁøÀûÀÎ º¯È­´Â ¿À´Ã³¯ÀÇ ±âÈÄ¿¡¼­µµ °¡´ÉÇÒ °ÍÀ¸·Î °£Áֵǰí ÀÖ´Ù. ÀÌ·¯ÇÑ ºùÇÙÀÇ º¯È­´Â ºÏ´ë¼­¾ç ÁÖº¯ÀÇ ±âÈĸ¦ ´ëÇ¥ÇÏ´Â °ÍÀ¸·Î ÁüÀ۵ǹǷÎ, ±âÈÄ ¿¬±¸ÀÚµéÀº Áö±¸¿Â³­È­·Î ÀÎÇØ ÇöÀçÀÇ ±âÈİ¡ ¹Ì·¡¿¡µµ ºñ½ÁÇÑ º¯È­¸¦ °ÞÀ» ¼ö ÀÖÀ½À» µÎ·Á¿öÇϰí ÀÖ¾ú´Ù.[20] ÇöÀç, ±×µéÀº ºùÇÙÀÇ ¸Ç ¾Æ·¡¿¡ ÀÖ´Â ÀÌ·¯ÇÑ Áøµ¿µéÀ» ¼³¸íÇϱâ À§Çؼ­, ±×·¯ÇÑ Ä¡¸íÀûÀÎ ±âÈÄ º¯È­¸¦ ÀÏÀ¸Ä×´ø ¾î¶² Á¾·ùÀÇ ¸ÞÄ¿´ÏÁòÀ» ÇÊ»çÀûÀ¸·Î ã°í ÀÖ´Ù. ±×µéÀº ºÏ´ë¼­¾ç¿¡¼­ÀÇ ÇØ·ùÀÇ Áߴܰú °°Àº ¸î °¡Áö °¡´É¼ºÀ» °í·ÁÇϰí ÀÖ´Ù. ÇÏÁö¸¸, ´Ù¸¥ °úÇÐÀÚµéÀº ±×¸°¶õµå ºù»óÀÇ ¸Ç ¹Ø¹Ù´ÚÀÌ ºù»ó È帧¿¡ ÀÇÇØ ¹æÇظ¦ ¹Þ¾Ò°í, µû¶ó¼­ ±× Áøµ¿Àº ±âÈÄÀûÀ¸·Î ¹«ÀǹÌÇÏ´Ù°í ¹Ï°í ÀÖ´Ù.

¹Ý¸é¿¡ âÁ¶·Ð ¸ðµ¨¿¡¼­´Â ºùÇϱ⠺κп¡¼­³ª °£ºù±â·Î ÁüÀ۵Ǵ ³·Àº ºÎºÐ¿¡¼­ÀÇ ±×·¯ÇÑ ±Þ°ÝÇÑ Áøµ¿Àº ¿¬·ûÃþÀÇ º¯µ¿ ¶Ç´Â ¼ö½Ê ³â ¸¸ÀÇ ±Þ°ÝÇÑ ¿Âµµ º¯È­°¡ ¾Æ´Ñ, ¼ºÃþ±Ç¿¡¼­ÀÇ ´Ù¾çÇÑ ¾çÀÇ È­»ê ºÐÁø°ú ¿¬¹«Áú(aerosol)¿¡ ÀÇÇÑ º¯È­¸¦ ³ªÅ¸³»´Â °ÍÀ̶ó°í º¸´Â °ÍÀÌ´Ù. À̰ÍÀº âÁ¶·ÐÀÚµéÀÌ ÃßÁ¤ÇÏ´Â ¿¬·ûÃþÀÇ µÎ²²°¡ ºùÇÙÀÇ ÀÌ ºÎºÐ¿¡¼­ ÈξÀ ´õ µÎ²®±â ¶§¹®ÀÌ´Ù. ±×·¯¹Ç·Î ¿ì¸®´Â °¡±î¿î Àå·¡¿¡ Àç¾ÓÀûÀÎ ±âÈÄ º¯È­ÀÇ °¡´É¼ºÀ» µÎ·Á¿öÇÒ Çʿ䰡 ¾ø´Ù.


Footnotes
1. Meese, D.A., A.J. Gow, R.B. Alley, G.A. Zielinski, P.M. Grootes, K. Ram, K.C. Taylor, P.A. Mayewski, and J.F. Bolzan, The Greenland ice sheet project 2 depth-age scale: Methods and results, Journal of Geophysical Research 102(C12):26411–26423, 1997.
2. Vardiman, L., Ice Cores and the Age of the Earth, Institute for Creation Research, El Cajon, CA, 1993.
3. De Angelis, M., J.P. Steffensen, M. Legrand, H. Clausen, and C. Hammer, Primary aerosol(sea salt and soil dust) deposited in Greenland ice during the last climatic cycle: Comparison with east Antarctic records, Journal of Geophysical Research 102(C12):26,683, 1997.
4. De Angelis, et al., Primary aerosol.
5. Oard, M.J., Do Greenland Ice Cores Show over One Hundred Thousand Years of Annual Layers? TJ 15(3):39–42, 2001.
6. Oard, Do Greenland Ice Cores. Oard, M.J., Are polar ice sheets only 4,500 years old? Acts and Facts Impact Article #361, Institute for Creation Research, El Cajon, CA, pp. i–iv, 2003. Oard, M.J., The Greenland and Antarctic ice sheets: Old or young? Institute for Creation Research, El Cajon, CA, 2004.
7. Oard, Greenland and Antarctic ice sheets.
8. Alley, R.B., et al., Visual-stratigraphic dating of the GISP2 ice core: Basis, reproducibililty, and application, Journal of Geophysical Research 102(C12):26378, 1997.
9. Oard, Greenland and Antarctic ice sheets.
10. Oard, Greenland and Antarctic ice sheets.
11. Bamber, J.L., R.L. Layberry, and S.P. Gogineni, A new ice thickness and bed set for the Greenland ice sheet 1, measurements, data reduction, and errors, Journal of Geophysical Research 106 (D24):33773–33780, 2001.
12. Bamber, J.L., and P. Huybrechts, Geometric boundary conditions for modeling the velocity field of the Antarctic ice sheet, Annals of Glaciology 23:364–373, 1996. Vaughan, D.G., J.L. Bamber, M. Giovinetto, J. Russell, and A.P. Cooper, Reassessment of net surface mass balance in Antarctica, Journal of Climate 12:933–946, 1999. Huybrechts, P., D. Steinhage, F. Wilhelms, and J. Bamber, Balance velocity and measured properties of the Antarctic ice sheet from a new compilation of gridded data for modeling, Annals of Glaciology 30:52–60, 2000.
13. Thomas, R.H., and PARCA investigators, Program for Arctic Regional Climate Assessment(PARCA): Goals, key finds, and future directions, Journal of Geophysical Research 106(D24):33692, 2001. Bales, R.C., J.R. McConnell, E. Mosley-Thompson, and B. Csatho, Accumulation over the Greenland ice sheet from historical and recent records, Journal of Geophysical Research 106 (D4):33, 813–833, 2001.
14. Huybrechts, P., D. Steinhage, F. Wilhelms, and J. Bamber, Balance velocity and measured properties of the Antarctic ice sheet from a new compilation of gridded data for modeling, Annals of Glaciology 30:56, 2000.
15. Bloomberg, R., WW II planes to be deiced, Engineering Report, March 9, 1989.
16. De Angelis, et al., Primary aerosol.
17. Oard, M.J., Wild Ice-Core Interpretations by Uniformitarian Scientists, TJ 16(1):45–47, 2002.
18. Hammer, C., P.A. Mayewski, D. Peel, and M. Stuiver, Preface to special volume on ice cores, Journal of Geophysical Research 102(C12):26315–26316, 1997.
19. Schulz, M., On the 1,470-year pacing of Dansgaard-Oeschger warm events, Paleoceanography 17(4):1–10, 2002.
20. Oard, M.J., The greenhouse warming hype of the movie The Day after Tomorrow, Acts and Facts Impact Article #373, Institute for Creation Research, El Cajon, CA, pp. i–iv, 2004.

 


URL : https://answersingenesis.org/environmental-science/ice-age/do-ice-cores-show-many-tens-of-thousands-of-years/
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1. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 11Àå ´Ü ÇÑ ¹øÀÇ ºùÇϱâ (Frozen in Time, Chapter 11. Only One Ice Age)
2. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 10Àå ºùÇϵéÀÇ °Ýº¯Àû À¶ÇØ (Frozen in Time, Chapter 10. Catastrophic Melting)
3. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 9Àå ºùÇϱâÀÇ ÀýÁ¤ (Frozen in Time, Chapter 9. The Peak of the Ice Age)
4. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 8Àå : Æø¼³ (Frozen in Time, Chapter 8. The Snowblitz)
5. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 7Àå : â¼¼±â ´ëÈ«¼ö¿¡ ÀÇÇØ ¿øÀÎµÈ ºùÇϱâ (Frozen in Time, Chapter 7. The Genesis Flood caused the Ice Age)
6. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 6Àå : ºùÇϱ⿡ ´ëÇÑ ¸¹Àº À̷еé°ú ¹®Á¦Á¡µé (Frozen in Time, Chapter 6. The Multiplication of Ice Age Theories)
7. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 5Àå : ¸êÁ¾ ÀüÀï ; ¸êÁ¾ÀÇ ¿øÀÎÀº ±âÈĺ¯È­? °ú´Ù»ìÀ°? (Frozen in Time, Chapter 5. The Extinction Wars)
8. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 4Àå : ¸Å¸Óµå¿¡ °üÇÑ ¸¹Àº °¡¼³µé (Frozen in Time, Chapter 4. A Mammoth Number of Mammoth)
9. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 3Àå : ºùÇϱâÀÇ ¹Ì½ºÅ͸® (Frozen in Time, Chapter 3. The Mystery of the Ice Age)
10. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 2Àå : ¿Ö ½Ãº£¸®¾Æ¿¡ »ì¾ÒÀ»±î? (Frozen in Time, Chapter 2. Why Live in Siberia?)
11. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. 1Àå : ½Ãº£¸®¾Æ¿¡ ¾ó¾îºÙÀº ¸Å¸Óµå »çüµé (Frozen in Time, Chapter 1. Frozen mammoth carcasses in Siberia)
12. ºùÇϱâ Ž±¸ - ¸ØÃç¹ö¸° ½Ã°£. ¼­·Ð (Frozen in Time, Preface)
13. ºùÇϱ⸦ ÃÊ·¡ÇÑ ³ë¾ÆÀÇ È«¼ö (Setting the Stage for an Ice Age)
14. À¯È¿ÇÏÁö ¾ÊÀº ¹Ð¶õÄÚºñÄ¡ ºùÇϱâ ÀÌ·Ð ³í¹®ÀÇ ±â³äÀÏÀ» À¯¸í °úÇÐ ÀâÁö´Â ÃàÇÏÇϰí ÀÖ¾ú´Ù. ('Big Science' Celebrates Invalid Milankovitch Paper)
15. ¹Ð¶õÄÚºñÄ¡ Áֱ⿡ ÀÇÇÑ ºùÇϱâ ÀÌ·ÐÀÌ ºÎÁ¤µÇ¾ú´Ù. (Orbital Ice Age Theory Melts)
16. ´ë¾çÀú ÅðÀû¹° ¿¬±¸¿Í ºùÇϱâ (Seafloor Sediment Research: Nearing Completion)
17. ȲÅä(·Ú½º)ÀÇ ±â¿ø°ú ³ë¾ÆÈ«¼ö, ±×¸®°í ÇÑ ¹øÀÇ ºùÇϱâ (Loess problems)
18. µÎÅÍ¿î ºù»ó(´ë·úºùÇÏ)Àº ¼ö½Ê¸¸ ³â¿¡ °ÉÃÄ Çü¼ºµÇ¾ú´Â°¡? (Thick Ice Sheets: How Old Are They Really?)
19. °í´ëÀÇ °Å´ëÇÑ ºù»ê°ú ºùÇϱâ, ±×¸®°í ³ë¾ÆÀÇ È«¼ö (Bible May Solve Colossal Ancient Iceberg Riddle)
20. °í´ë È£¼ö ÅðÀûÃþ°ú ±âÈÄ º¯È­, ±×¸®°í ¼º°æÀû ´Ü¼­ (Ancient Lake Bed Merges with Biblical Clues)
21. ºùÇϱâ¿Í â¼¼±â È«¼ö (The Ice Age and the Genesis Flood)
22. ¿©·¯ ¹øÀÇ ºùÇϱâ À̷аú ¸ð¼øµÇ´Â ºü¸¥ ºùÇÏ ¼Óµµ. (Speedy Glaciers Trample Multiple Ice-Age Theories)
23. °ú°Å ±âÈÄ º¯È­ÀÇ ÇÑ ÁöÇ¥¿´´ø ºùÇÙÀº ºÎÁ¤È®ÇÒ ¼ö ÀÖ´Ù. (Scientific Markers Can Mislead 1)
24. ºùÇϱ⠸»¿¡ ÀÖ¾ú´ø µÎ ¹øÀÇ °Å´ë È«¼ö°¡ ¹ß°ßµÇ¾ú´Ù. (Two more late Ice Age megafloods discovered)
25. ¹Ì¶ó°¡ µÈ ½£°ú ´ëÈ«¼ö ÀÌÈÄ ºùÇϱâ (Mummified Forest Highlights Post-Flood Ice Age)
26. ±Þ¼ÓÈ÷ ÁúÁÖÇß´ø ºùÇϵé (Galloping Glaciers)
27. µ¿ÀϰúÁ¤¼³ °úÇÐÀÚµéÀÇ ¹ÏÀ» ¼ö ¾ø´Â ¾óÀ½ ÄÚ¾î ÇØ¼® (Wild ice-core interpretations by uniformitarian scientists)
28. ºùÇϱâ¿Í ±×¿¡ µû¸¥ ¹®Á¦Á¡µé 2
29. ºùÇϱâ¿Í ±×¿¡ µû¸¥ ¹®Á¦Á¡µé 1
30. °í´ëÀÇ ¾óÀ½ (Ancient Ice) 1
31. °í´ëÀÇ ¾óÀ½ (Ancient Ice) 2
32. ¾óÀ½ ¼Ó¿¡ ¹¯ÇôÀÖ´ø ºñÇà±â°¡ ´Ù½Ã ³¯´Ù! (Ice-bound plane flies again!)
33. ¿­´ë ´Ù¿ì¸² È­¼®µéÀº ±ØÀûÀÎ ±âÈÄ º¯È­¸¦ Áõ°ÅÇϰí ÀÖ´Ù. (Rainforest Fossils Demonstrate Dramatic Climate Change)
34. ¸Å¸Óµå ¸êÁ¾ÀÇ ¹Ì½ºÅ͸®°¡ ¸¶Ä§³» Ç®·È´Â°¡? (Wooly Mammoth Mystery Finally Solved?)
35. ¸Å¸Óµå´Â »ý°¢Çß¾ú´ø °Íº¸´Ù ÃÖ±Ù±îÁö »ì¾Ò´Ù. (Mammoths Were Alive More Recently than Thought)
36. ´ÙÀ̾Ƹóµå´Â ¸Å¸ÓµåµéÀÇ Á×À½¿¡ ´Ü¼­¸¦ Á¦°øÇϴ°¡? (Diamond Clues to Beasts¡¯ Demise)
37. µ¿°áµÈ »õ³¢ ¸Å¸Óµå°¡ ¿Ïº®ÇÑ »óÅ·Π¹ß°ßµÇ¾ú´Ù. (Baby Frozen Mammoth Found Intact)
38. ÀÌÁýÆ®ÀÇ ¹Ù·Îµé »çÀÌ¿¡ ¸Å¸Óµå? (Mammoth among the pharaohs?)
39. ÇÑ ºùÇϱ⠿¬±¸ÀÚ°¡ ¸Å¸Óµå ½Åºñ¸¦ Ç®¾ú´Ù. (¡°Mr. Ice Age¡± solves woolly mammoth mystery)
40. ¼ö¹é¸¸ ¸¶¸®ÀÇ ¸Å¸Óµå È­¼®Àº ¾î¶»°Ô Çü¼ºµÇ¾ú½À´Ï±î? (How did millions of mammoth fossils form?)
41. ¾ó¾îºÙÀº ¸Å¸Óµå (Frozen mammoths)
42. ¸Å¸Óµå - ºùÇϱâÀÇ ¼ö¼ö²²³¢ (Mammoth - Riddle of the Ice Age)
43. ºÏ±Ø Áö¹æÀÇ È¤¼­±â (Arctic Heat Wave)
44. È­¼® ¾Æ¸Þ¸®Ä« »ï³ª¹«´Â ºÏ±Ø¿¡¼­ ¹«¾ùÀ» Çϰí ÀÖ¾ú´Â°¡? (What Are Fossil Redwoods Doing in the Arctic?)
45. ³²±Ø´ë·úÀÇ ºù»ó ¾Æ·¡¿¡ °Å´ëÇÑ Çù°îµéÀÌ Á¸ÀçÇÑ´Ù. (Possible Super-Grand Canyon Found Under Antarctica)
46. ³²±Ø¿¡¼­ ¿­´ë ³ª¹« È­¼®ÀÌ ¹ß°ßµÇ¾ú´Ù. (Tropical Trees Found in Antarctica)
47. °ú°Å ³²±Ø¿¡ ¾ßÀÚ¼ö°¡ ¹ø¼ºÇß´Ù. (Palm Trees Thrived in Antarctica)
48. ³²±Ø¿¡¼­ ¹ß°ßµÈ °í´ë À̳¢¿Í °ïÃæµé (Ancient Moss, Insects Found in Antarctica)
49. °ú°Å ±×¸°¶õµå´Â Ǫ¸¥ ½£À̾ú´Ù. (Greenland Was Forest Green)
50. ±×¸°¶õµå ¾óÀ½ ¾Æ·¡ 3.2 km ±íÀÌ¿¡¼­ ½Ä¹°µéÀÌ ¹ß°ßµÇ¾ú´Ù (Plant Found Two Miles Under Greenland Ice)
51. ÀÒ¾î¹ö¸° ºñÇàÁß´ë (The Lost Squadron)
52. ±×¸°¶õµå ¾óÀ½ 91m ¾Æ·¡¿¡¼­ Á¦2Â÷ ¼¼°è´ëÀü ¶§ÀÇ ¡®ÀÒ¾î¹ö¸° ºñÇàÁߴ롯ÀÇ ¶Ç ´Ù¸¥ ºñÇà±â°¡ ¹ß°ßµÇ¾ú´Ù. (WW2 Aircraft Found Under 300 Ft of Greenland Ice)
 
 
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