• Bulletin of the Korean Space Science Society
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• 2009.10a
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• pp.44.2-44.2
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• 2009

한국천문연구원 태양우주환경연구그룹은 우주환경예 경보 연구에 활용하기 위하여 일본 Tierra Tecnica사의 RFP-523C 지자기 측정 시스템을 보현산천문대 태양망원경동에 구축하였다. 보현산 지자기 측정 시스템은 2007년 11월에 구축이 완료되어 현재 우주환경 변화에 의한 지자기 변화를 측정 및 저장하고 있다. 보현산 지자기 측정 시스템으로 측정한 지자기 자료를 사용하여 2008년부터 2009년 8월까지 보현산 지역의 지자기 일변화와 연변화를 연구하였다. 지자기 일변화와 연변화는 태양활동에 의한 영향을 받아 변화하는데, 지자기 일변화는 K 지수를 산출하는데 사용되고 지자기 연변화는 보현산 지역의 장기간 동안의 지자기 변동을 연구하는데 사용된다.

• Journal of Forest and Environmental Science
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• v.23 no.1
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• pp.29-33
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• 2007

This study was purposed to elucidate the best optimum sites by ecophysiological response measurements of Kalopanax pictus samplings of plantation. The diurnal changes of the stomatal transpiration, water use efficiency, water potential, and intercellullar $CO_2$ concentration of leaves were measured by the portable IR $CO_2$ analyzer. The results obtained are summarized as follows. 1) The daily stomatal transpiration rate was highest at 10:00 a.m. After 16:00, the stomatal transpiration rate rapidly decreased. 2) The daily water use efficiency was maximum at 8:00 a.m., and then rapidly decreased until midday with decreasing water potential. 3) The daily $C_i/C_a$ ratio rapidly decreased until 9:00 a.m., and then showed a stable value until 16:00, and then rapidly increased. The daily intercellullar $CO_2$ concentration ($C_i/C_a$ ratio) showed the same tendency as water potential changes. Consequently, stomatal transpiration and water use efficiency was increased with high water potential of leaves at am, and then remarkably decreased with low water potential at pm.

• Journal of Astronomy and Space Sciences
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• v.23 no.2
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• pp.117-126
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• 2006

The Diurnal variation of galactic cosmic ray (GCR) flux intensity observed by the ground Neutron Monitor (NM) shows a sinusoidal pattern with the amplitude of $1{\sim}2%$ of daily mean. We carried out a statistical study on tendencies of the local times of GCR intensity daily maximum aad minimum. To test the influences of the solar activity and the location (cut-off rigidity) on the distribution in the local times of maximum and minimum GCR intensity, we have examined the data of 1996 (solar minimum) and 2000 (solar maximum) at the low-latitude Haleakala (latitude: 20.72 N, cut-off rigidity: 12.91 GeV) and the high-latitude Oulu (latitude: 65.05 N, cut-off rigidity: 0.81 GeV) NM stations. The most frequent local times of the GCR intensity daily maximum and minimum come later about $2{\sim}3$ hours in the solar activity maximum year 2000 than in the solar activity minimum you 1996. Oulu NM station whose cut-off rigidity is smaller has the most frequent local times of the GCR intensity maximum and minimum later by $2{\sim}3$ hours from those of Haleakala station. This feature is more evident at the solar maximum. The phase of the daily variation in GCR is dependent upon the interplanetary magnetic field varying with the solar activity and the cut-off rigidity varying with the geographic latitude.

• Korean Journal of Agricultural and Forest Meteorology
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• v.11 no.4
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• pp.247-251
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• 2009

To estimate the effect of rainfall on soil respiration, soil $CO_2$ efflux was measured with a manipulation of rainfall interception at a broad-leaved deciduous forest in western Japan from 20 February to 19 November 2001. The diurnal patterns of soil respiration observed at the intercepted subplot ($F_c$) were quite similar to those of soil temperature at 0.2 m depth with a maximum around midnight and a minimum from noon to early afternoon. Such diurnal patterns have not been observed in the previous studies at the same study site under natural conditions (which manifested no clear diurnal variations). Furthermore, the magnitudes of $F_c$ showed substantial differences (e.g., ~50% reduction under water-limited conditions) compared to those of the potential soil respiration under natural conditions ($F_{cal}$). These findings demonstrate that rainfall events not only affected the magnitude of soil $CO_2$ efflux but also modified the vertical structure of soil temperature, thereby altering diurnal patterns of soil respiration.

• Geophysics and Geophysical Exploration
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• v.12 no.2
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• pp.208-214
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• 2009

Using the GNSS data and tilt-meter data of Boeun (BOEN) and Goesan (GSAN) GNSS stations, we have calculated the differential distance vector variation with the calculation time span set to 1 hour and 3 hour and differential tilt vector variation along time and derived an indicator of similarity between the two variations along time. The similarity such calculated is rather lower than high. But as the existence of a circular type movement of the antenna's phase center's location due to the tilt's variation of the antenna tower because of the sunlight's diurnal change is certain, we recommend to take such diurnal variation of antenna's location into consideration when the correction error in DGNSS or the measured data at reference stations in VRS (Virtual Reference System) is broadcast.

• Proceedings of the Korean Society of Crop Science Conference
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• 1981.10a
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• pp.9-9
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• 1981

• Proceedings of the Zoological Society Korea Conference
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• 1995.10b
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• pp.210.2-210
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• 1995

• Proceedings of the Zoological Society Korea Conference
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• 1997.10b
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• pp.124.2-124
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• 1997

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2003.05a
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• pp.219-222
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• 2003

2002년 3월 28일과 29일에 동해 울릉도에서 존데를 이용하여 관측한 자료와 AWS 자료 등을 이용하여 얻은 이상의 결과를 요약하면 다음과 같다. 일반적인 경우와는 달리 주간에 형성된 혼합층이 일몰 후 야간까지 소멸하지 않았다. 그 이유는 구름으로부터 방출되는 장파복사로 인한 열속(heat flux)이 하층대기를 가열시켜 오히려 기온을 증가시키기 때문이다. 따라서 혼합층은 지면의 열속의 영향을 절대적으로 받는다. 또한 혼합층의 발달과 소멸에 있어서 구름의 영향을 무시할 수 없으며, 구름의 유무에 따라 대기경계층의 일변화는 많은 차이를 나타낸다. 구름 유무에 따른 지속적인 관측이 이루어진다면 더 자세한 영향을 알 수 있을 것이며, 더 나아가 해양대기경계층의 특성 연구에 도움을 줄 것으로 생각된다.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2005.11a
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• pp.268-269
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• 2005