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[¿À¼¼¾Æ´Ï¾Æ] [2014] [È£ÁÖ] Çؼö ¿Âµµ¸¦ ½Ç½Ã°£À¸·Î Æǵ¶ÇÏ´Â »õ·Î¿î ¸ðµ¨
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[È£ÁÖ] Çؼö ¿Âµµ¸¦ ½Ç½Ã°£À¸·Î Æǵ¶ÇÏ´Â »õ·Î¿î ¸ðµ¨

¼­ºÎ È£ÁÖ ¿¬±¸ÁøÀº Çؾ纸ȣ¼ö¿ª(MPAs; marine protected areas)¿¡ ´ëÇØ ±Ù½Ç½Ã°£(near real-time)À¸·Î Áö¿ªÀûÀÎ ¼ö¿Â(water temperature)À» Á¤È®ÇÏ°Ô ÃßÁ¤ÇÏ´Â ¸ðµ¨À» óÀ½À¸·Î °³¹ßÇß´Ù. ÀÌ ¸ðµ¨Àº ¼ö¿Â¿¡¼­ ´Ù¾çÇÑ °èÀý À¯ÇüÀ» ¸ðÇüÈ­ÇÏ´Â °ÍÀÌ °¡´ÉÇϱ⠶§¹®¿¡, ´Ù¸¥ ¸ðµ¨º¸´Ù ´õ Á¤È®ÇÏ´Ù.

¿¬±¸ÆÀÀº ¹Ì±¹ ±¹¸³ ÇØ¾ç ´ë±â °ü¸®Ã³(NOAA; National Oceanic and Atmospheric Administration)ÀÇ CRW(Coral Reef Watch) ÇÁ·Î±×·¥À¸·ÎºÎÅÍ Çؼö¸é ¿Âµµ(SST; sea surface temperature)¿Í ¸ðµ¨À» Å×½ºÆ®Çϱâ À§ÇÏ¿© 4°÷ÀÇ ¼­ºÎ È£ÁÖ MPAs·ÎºÎÅÍ ¾òÀº ÇöÀå ¿Âµµ(in situ temperature)¸¦ »ç¿ëÇß´Ù.

CRW´Â ÇØ¾ç °ü¸®ÀÚ¿Í ¿¬±¸ÁøÀÌ Àü ¼¼°èÀûÀ¸·Î ±Ù½Ç½Ã°£ SST °»½Å¿¡ ´ëÇÑ Á¢±ÙÀ» Á¦°øÇÑ´Ù. ¼­È£ÁÖ °ø¿ø ¹× ¾ß»ý »ý¹°ºÎ(Western Australian Department of Parks and Wildlife) ¼Ò¼ÓÀÇ ¿¬±¸ °úÇÐÀÚÀÎ Kevin Bancroft´Â »õ·Î¿î ¸ðµ¨ÀÌ ÇØ¾ç »ý¹°¿¡ ´ëÇÑ ¿­Àû º¯Ä¢¼º(thermal anomalies)À» ÀÌÇØÇϴµ¥ µµ¿òÀ» ÁÙ °ÍÀ̶ó°í ¹àÇû´Ù.

* »êÈ£ Å»»ö Çö»óÀ» ¾Ï½ÃÇÏ´Â ¿Âµµ ¸ðµ¨
Bancroft´Â ±¤¹üÀ§ÇÑ »êÈ£ Å»»ö(coral bleaching)ÀÇ ¹ß»ýÀÌ 2010³â~2011³â°ú 2011³â~2012³â ¿©¸§Ã¶ µ¿¾È ³ôÀº ¼ö¿ÂÀÌ ³ªÅ¸³­ Á÷Á¢ÀûÀÎ °á°ú¶ó°í ¹àÇû´Ù. °ú°Å¿¡, ¿ì¸®´Â CRW°¡ »êÈ£ Å»»ö »ç°Ç¿¡ ´ëÇÑ ÀÇ°ßÀÌ Á¦½ÃµÆÀ» ¶§, Á¾Á¾ Å»»ö »ç°ÇÀ» È®ÀÎÇÏÁö ¸øÇß´Ù´Â »ç½ÇÀ» ¹ß°ßÇß´Ù°í ±×´Â ¹àÇû´Ù.

¼ö¿ÂÀÌ Á¾Á¾ Çؾȿ¡¼­ ÃøÁ¤µÇ±â ¶§¹®¿¡ ¿ì¸®¿¡°Ô °æ°í¸¦ ÁØ ½Ã±â¿Í´Â ´Ù¸¥ ¶§, Å»»ö »ç°ÇÀÌ ±â·ÏµÆ´Ù. ÀÌ·¯ÇÑ ¿ÀÂ÷¸¦ ÇØ°áÇϱâ À§ÇÏ¿©, ¿¬±¸ÁøÀº »ç¶÷µéÀÌ °ú°Å¿¡ Á¤±âÀûÀ¸·Î ¿Âµµ¸¦ ±â·ÏÇÏ´ø ±â·Ï º¸°ü¼ÒÀÇ ÀڷḦ Á¶¸íÇßÀ¸¸ç, ´Ù¾çÇÑ MPAs¿¡¼­ ÀÚüÀûÀÎ ±â·ÏÀ» È®º¸Çß´Ù. Bancroft´Â ÇöÀç ¼­È£ÁÖÀÇ MPAs Àü¿ªÀÇ ´Ù¾çÇÑ À§Ä¡¿¡ ´ëÇÑ ¿Âµµ ¸ðµ¨À» È®º¸ÇßÀ¸¸ç, ´Ù¸¥ Áö¿ª¿¡ ´ëÇÏ¿© ÀÌ·¯ÇÑ ¸ðµ¨À» È®ÀåÇϱâ À§ÇÑ °³¼±À» ¼öÇàÇÏ°í ÀÖ´Ù°í ¹àÇû´Ù.

* Çؼö¸é ¿ÂµµÀÇ ÀΰøÀ§¼º Æǵ¶
NOAA´Â ÇؾçÀÇ Àû¿Ü¼± º¹»ç(infrared radiation)¿Í ÀÌ¿¡ µû¸¥ ¿Âµµ¸¦ ÃøÁ¤Çϱâ À§ÇÏ¿© ÀΰøÀ§¼º °¨Áö±â(satellite sensor)¸¦ »ç¿ëÇß´Ù. 50km*50km Çȼ¿ÀÇ °¡»ó ¿µ¿ª(virtual area)Àº ¸®¼ÁÅϽº °ª(receptance value)À» ¹æÇØÇÒ ¼ö ÀÖ´Â ¼¶ ¶Ç´Â ´Ù¸¥ °ÍÀº Æ÷ÇÔÇÒ ¼ö ¾ø´Ù. ÀÌ°ÍÀÌ ¿Ö ÀÚ·á°¡ ÀüÇüÀûÀ¸·Î ÇؾÈÀ¸·ÎºÎÅÍ À¯·¡Çߴ°¡¿¡ ´ëÇÑ ÀÌÀ¯°¡ µÈ´Ù.

Bancroft´Â NOAA°¡ ÀΰøÀ§¼º ÀÚ·á·ÎºÎÅÍ 5km*5km Çȼ¿À» »ç¿ëÇÏ´Â º¸´Ù ´õ ºÐÇØ´ÉÀÌ ¿ì¼öÇÑ Çؼö¸é ¿Âµµ ¸ðµ¨À» °³¹ß ÁßÀ̶ó°í ¹àÇû´Ù. ÀÌ°ÍÀº MPAs À̳» ¶Ç´Â ÁÖº¯ÀÇ °¡»ó Áö¿ªÀÇ À§Ä¡¸¦ º¸´Ù ´õ °³¼±ÇÒ ¼ö ÀÖ´Ù´Â °ÍÀ» ÀǹÌÇÑ´Ù°í Bancroft´Â ¹àÇû´Ù.

Ãß°¡ÀûÀÎ ¹æÇâÀº À¥ ±â¹ÝÀÇ µµ±¸¸¦ ÀÌ¿ëÇÏ¿© ÇØ¾ç °ø¿ø °ü¸®ÀÚ¿¡°Ô ±Ù½Ç½Ã°£ ÀڷḦ Á¦°øÇÏ´Â °øÁ¤ÀÇ ÀÚµ¿È­¸¦ ¼öÇàÇÏ¿© º¸´Ù ´õ ¿ì¼öÇÑ °ü¸®¸¦ °áÁ¤Çϴµ¥ ÀÖ´Ù°í Bancroft´Â ¹àÇû´Ù.

Çؼö ¿Âµµ(sea temperature)ÀÇ ±Ù½Ç½Ã°£ °üÃøÀº ´Ù¾çÇÑ ÇØ¾ç ±ºÁý ƯÈ÷, MPAs¿¡ ´ëÇÑ ±âÈÄ º¯È­¿Í °ü·ÃµÈ ¿µÇâÀ» ¸ð´ÏÅ͸µÇϱâ À§ÇÑ Áß¿äÇÑ °ü¸® µµ±¸ÀÌ´Ù. ±×·¯³ª °¡»ó ±âÁö·Î ÀΰøÀ§¼º ¿ø°Ý °¨Áö(satellite remote sensing)·ÎºÎÅÍ À¯·¡ÇÑ ÀڷḦ ÀÌ¿ëÇÒ ¶§ Á¸ÀçÇÏ´Â ÇÑ°è´Â ÀϹÝÀûÀ¸·Î °ü¸®ÇÏ°íÀÚ °ü½ÉÀ» °¡Áø Áö¿ª°ú´Â °Å¸®°¡ ÀÖ´Ù. ´ëºÎºÐÀÇ Áö¿ª¿¡¼­ ¸ðÇüÈ­µÈ Çؼö¸é ¿Âµµ´Â ƯÁ¤ÇÑ ¿¹Ãøº¸´Ù´Â º¸´Ù ´õ Å« °ø°£Àû ±Ô¸ð¿¡ °ÉÃÄ ÀϹÝÀûÀÎ ¿¹Ãø¸¸À» Á¦°øÇÑ´Ù.

¿ø°Ý °¨ÁöµÈ Çؼö ¿Âµµ¿Í ÇöÀå ¿Âµµ »çÀÌÀÇ °ü°è¸¦ ÀÌÇØÇÏ´Â °ÍÀº Àå±âÀû º¯È­(long-term changes)¿Í ´Ü±âÀû º¯Ä¢¼º(short-term anomalies)¿¡ °üÇÏ¿© Çؼö ¿Âµµ¿¡ ´ëÇÑ ½Ç½Ã°£ °ü¸® ¹ÝÀÀÀ» °¡´ÉÇÏ°Ô ÇÑ´Ù. ¿ª»çÀûÀ¸·Î ÇØ¾ç ±ºÁý¿¡ ´ëÇÑ ´ëºÎºÐÀÇ ¿­ ½ºÆ®·¹½º »ç°Ç(thermal stress event)ÀÇ È¿°ú´Â ÇöÀå ±â·Ï°ú »ç°Ç, ȸ¼ö ¹× ÀÚ·á Çؼ® µî°ú °ü·ÃµÈ ½Ã°£ Áöü ¶§¹®¿¡, »ç°ÇÀÌ ÀϾ ÈÄ ¿ì¹ßÀûÀ¸·Î °üÂûµÇ°Å³ª Àß ±Ô¸íµÈ´Ù. ¿­ ½ºÆ®·¹½º »ç°ÇÀ¸·ÎºÎÅÍÀÇ º¹±Í¿Í ÇØ¾ç ±ºÁýÀÇ °¨¼ö¼ºÀ» ÀÌÇØÇÏ´Â °ÍÀº Áö¿ªÀû °ø°£ ±Ô¸ð¿¡¼­ ½Ç½Ã°£À¸·Î »ç°ÇÀÇ ½Å·Ú ÀÖ´Â ÃßÁ¤À» ÇÊ¿ä·Î ÇÑ´Ù.

ÇöÀåÀÇ Çؼö ¿Âµµ¿Í ÀΰøÀ§¼º¿¡¼­ À¯·¡ÇÑ Çؼö ¿Âµµ »çÀÌÀÇ °ü°è¸¦ Ãß°¡·Î ´õ ÀÌÇØÇÏ°í, ½Ç½Ã°£ ¸ð´ÏÅ͸µ µµ±¸¸¦ °³¹ßÇϱâ À§ÇÏ¿©, ´Ü¼øÇÑ ¼±Çü º¸°£¹ý(linear interpolation)ÀÌ ±Ù½Ç½Ã°£ ÀΰøÀ§¼º¿¡¼­ °üÃøµÈ Çؼö¸é ¿Âµµ¸¦ ÀÌ¿ëÇÏ¿© ±íÀÌ¿¡ µû¶ó Áö¿ªÀûÀÎ ÇöÀå ¿Âµµ¸¦ ÃßÁ¤Çϱâ À§ÇÏ¿© ¼öÇàµÆ´Ù.

NOAAÀÇ CRW(Coral Reef Watch) 50km Çؼö¸é ¿Âµµ(SST) ÀÚ·á´Â ½±°Ô ÀÌ¿ë °¡´ÉÇϸç, Àü ¼¼°èÀûÀ¸·Î Çؼö¸é ¿ÂµµÀÇ ¿¬¼ÓÀûÀÎ ½Ç½Ã°£¿¡ °¡±î¿î °»½ÅÀ» ÀÌÀ¯·Î ¼±ÅõƴÙ. ¶Ç 4°÷ÀÇ ¼­È£ÁÖ MPAs·ÎºÎÅÍ ÇöÀå ¿Âµµ ÀÚ·á Áý·Ï ÀåÄ¡(logger data)°¡ ¼±Çü º¸°£¹ýÀ» °³¹ßÇÏ°í Å×½ºÆ®Çϴµ¥ ÀÌ¿ëµÆ´Ù.

¸ðµ¨À» ÀÌ¿ëÇÏ¿©, ¿¬±¸ÁøÀº 4°÷ÀÇ MPA Àü¿ªÀÇ °ü½ÉÀÌ ÀÖ´Â Áö¿ª¿¡¼­ 2011³â 2¿ù¿¡ °æÇèÇß´ø ¿Âµµ º¯Ä¢¼ºÀ» Æ÷ÇÔÇÏ¿©, ÃÖ¼Ò 78%ÀÇ ½Ã°£¿¡ ´ëÇÏ¿© ¡¾1 ¡ÆC À̳»·Î ÇöÀå ¿Âµµ¸¦ ¼º°øÀûÀ¸·Î ÃßÁ¤ÇÒ ¼ö ÀÖ¾ú´Ù.

ÀÌ·¯ÇÑ ´Ü¼øÇÑ ¼±Çü º¸°£¹ý ¸ðµ¨(linear interpolation model)Àº ¼­È£ÁÖ Àü¿ªÀÇ ±¤¹üÀ§ÇÑ ¹üÀ§ÀÇ MPAs ¸ð´ÏÅ͸µÀ» À§ÇÏ¿© ¿ÂµµÀÇ ½Ç½Ã°£ ÃßÁ¤À» °³¼±Çϱâ À§ÇÏ¿© »ç¿ëµÉ °èȹÀÌ´Ù. ÀÌ·¯ÇÑ ¼±Çü º¸°£¹ý ¸ðµ¨Àº Àå±âÀûÀÎ º¯È­¿Í ´Ü±â ±â¿Â º¯Ä¢¼º¿¡ ´ëÀÀÇÑ ¸¹Àº Á¤º¸¸¦ °®Ãá °ü¸®¿Í ´õ ¿ì¼öÇÑ ÀÌÇظ¦ °¡´ÉÇÏ°Ô ÇÒ °ÍÀÌ´Ù.

¸ð´ÏÅ͸µµÇ´Â Áö¿ªÀÇ Ãß°¡ÀûÀÎ È®´ë, °³¼±µÈ ÀΰøÀ§¼º ºÐÇØ´É ¹× ÀÚ·á °ø±Þ¿øÀÇ ¿¬°£ °ËÅä µîÀÌ ÀÌ¿ë °¡´ÉÇÑ ÀÚ·á¿Í ÇÔ²² ³ôÀº ¼öÁØÀÇ Á¤È®µµ¿¡¼­ ³²¾Æ ÀÖ´Â ¼öÁú¿¡ ´ëÇÑ ÀÌ·¯ÇÑ À§ÇùÀ» °ü¸®Çϴµ¥ »ç¿ëµÇ´Â ÀڷḦ È®º¸ÇÒ °ÍÀÌ´Ù.

±×¸²1> ÇؾçÀÇ Àû¿Ü¼± º¹»ç¿Í ÀÌ¿¡ µû¸¥ ¿Âµµ¸¦ ÃøÁ¤Çϱâ À§ÇÏ¿© ÀΰøÀ§¼º °¨Áö±â(satellite sensor)¸¦ »ç¿ëÇÏ´Â ¹Ì±¹ ±¹¸³ ÇØ¾ç ´ë±â °ü¸®Ã³(NOAA; National Oceanic and Atmospheric Administration)

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Sea temperatures likely readable real-time with new model

Western Australian researchers believe they are first to develop a model for accurately estimating local water temperature in near real-time for marine protected areas (MPAs).
The model is more accurate than others because it allows for different seasonal patterns in water temperature. The group used sea surface temperature (SST) data from the US National Oceanic and Atmospheric Administration's (NOAA) Coral Reef Watch (CRW) program and in situ temperature data from four WA MPAs to test the model.

The CRW provides marine managers and researchers with access to near real-time SST updates globally.
Department of Parks and Wildlife research scientist Kevin Bancroft says the model will help in understanding thermal anomalies on marine life.

Temperature model could indicate coral bleaching events

Mr Bancroft says extensive coral bleaching was a direct result of the high water temperatures during summer in 2010–11 and 2011–12.
"In the past we've noticed that when the CRW has issued a bleaching event, we've often found that there hasn't been a bleaching event," he says. "Other times when they haven't alerted us, bleaching events have been recorded—that's because the water temperatures they're measuring are offshore.
"To correct this, we've looked at archival data where people have logged temperature regularly in the past and we've had our own loggers out in various MPAs as well."

Mr Bancroft says he now has a temperature model for various sites throughout WA's MPAs and would like to improve the spread of these models for other sites.
"At least if we get a bleaching event, we can go to NOAA, download their data, whack it in the model and come out with an estimated in situ water temperature for that particular site, and it will inform us on whether we need to put in some management strategy," he says.

Satellite sensors reading the ocean's surface temperature

NOAA uses a satellite sensor to measure infrared radiation of the ocean, and thus its temperature.
This virtual area of 50km by 50km pixels cannot include islands or anything that will interfere with the receptance value; this is why the data is typically from offshore.
Mr Bancroft says NOAA is developing a finer resolution sea surface temperature model using 5km by 5km pixels from their satellite data.

"This means we'll be able to refine the locations of virtual sites within and around MPAs," he says.
"Future directions would involve the automation of the process of providing near real-time data to marine park managers via a web-based tool, to enable better management decisions."
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