• 대기
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• 제26권1호
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• pp.73-84
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• 2016

A method to make ice spike using home refrigerator with ice tray was found. Many experiments have carried out with this method and many natural phenomena occurring on the formation of ice spike are found. A new concept of the Latter Freezing Water (LFW) was imported to explain the ice spike formation. At LFW position on water surface, the Sprout of Super cooled Water (SSW) grows by the Volume Expansion Effect (VEE) caused by the phase change of water in water. And air bubbles that are expelled from ice during freezing process, gather, rise, and detonate at the upper most part of SSW that make SSW freeze and grow upward with the water pipe in it. Together with VEE the capillarity in the water pipe makes the column grow more, that makes the ice spike. Many other findings were succeeded; 1) Ice spike process is completed before the whole water freezes. 2) If water is corrupted or shocked, even though it is very slight, ice spike is not generated. 3) Rain water contains the most LFW among all kind of waters used in experiments. 4) LFW is changed into normal water after passing the ice spike. 5) A new concept of the ice bullet is introduced. 6) The reason of frequent occurrences of the ice spike at Mt. Mai is investigated also.

• 대기
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• 제20권4호
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• pp.427-436
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• 2010

The single-scattering optical properties of ice crystals in cirrus clouds by the aircraft measurement data were investigated, and the radiative equilibrium temperatures and radiative fluxes were calculated and analyzed by radiative convective model with the variations of ice crystal habits and sizes in cirrus clouds. The homogeneous cloud is assumed to be in the layer 200~260 hPa with an ice crystal content of $10gm^{-2}$ for the flux calculation. The profiles of temperature, humidity, and ozone typical of mid-latitude summer are used. The surface albedo is assumed to be 0.2 for all spectral bands and the cosine of solar zenith angles is 0.5. The result of radiative equilibrium temperature at surface was less than surface temperature of the standard atmosphere data in case of smaller effective ice crystal size and larger optical thickness. The column, aggregation and plate in 6 ice crystal habits were the most effective in positive greenhouse effect and bullet-4 was the worst in it. At the surface, the maximum difference of equilibrium temperature by 6 kinds of ice crystal habits were about 3~15 K with 30 sample aircraft measurement data.

• 대기
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• 제23권1호
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• pp.39-45
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• 2013

A parameterization for the scattering of longwave radiation by ice clouds has been developed based on spectral scattering property calculations with shapes and sizes of ice crystals. For this parameterization, the size distribution data by Fu (1996) and by Michell and Arnott (1994) are used. The shapes of ice crystal considered in this study are plate, solid column, hollow column, bullet-rosette, droxtal, aggregate, and spheroid. The properties of longwave scattering by ice crystals are presented as a function of the extinction coefficient, single-scattering albedo, and asymmetry factor. The heating rate and flux by the radiative parameterization model are calculated for wide range of ice crystal sizes, shapes, and optical thickness. The results are compared with the calculated results using a six-stream discrete ordinate scattering algorithm and Chou's method. The new method (with various habits and size distributions) provides a good simulation of the scattering properties and cooling rate in optically thin clouds (optical thickness < 5). Depending on the inclusion of scattering by ice clouds, the errors in the calculation of the cooling rates are significantly different.

• 한국마린엔지니어링학회:학술대회논문집
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• 한국마린엔지니어링학회 2011년도 전기공동학술대회 논문집
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• pp.322-322
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• 2011

본 연구는 동관의 관외착빙형 특성을 조사하기 위한 기초적인 연구로써, 실험의 파라메터와 범위는 브라인의 온도는 -10[$^{\circ}C$], -8[$^{\circ}C$], -6[$^{\circ}C$], 브라인의 유속은1.0[m/s], 1.4[m/s], 1.8[m/s] 그리고물의 초기온도는6[$^{\circ}C$], 9[$^{\circ}C$], 12[$^{\circ}C$] 등으로 설정하였다. 본 논문에서는 무차원 얼음 두께와 무차원 동결 시간의 관계에 대하여 실험적으로 정리 하였다. 브라인온도, 물의 온도, 브라인 유속, 물의 초기온도, 동관의 직경사이즈에 대한 무차원 상관 방정식은 다음과 같이 얻어진다. r+3 = $0.063{\bullet}(t+)+0.206$ [적용범위: R+T+=2.1~4.7].

• 한국수산과학회지
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• 제15권3호
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• pp.219-225
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• 1982

1) 2성분계 도지두부의 유효열전도도($\lambda_e$)를 $0\sim20^{\circ}C$ 및$-5\sim-20^{\circ}C$의 범위내에서 측정한 결과, 수분함양의 증감에 따라 $\lambda_e$값도 증감했으며, 동결점이상의 온도대에서는 온도의 상승과 함께 $\lambda_e$값도 커지고, 동결점 이하에서는 온도의 하강과 함께 $\lambda_e$값이 커졌다. 2) 3성분계 두부의 유효열전도는 수분함양이 증가함에 따라 $\lambda_e$값은 커져가나 지질의 함양이 증가함에 따라 $\lambda_e$값은 작아졌다. $\lambda_e$값의 온도의존성은 2성분계도지두부의 경우와 유사했다. 3)대대단백질의 고유열전도도는 미동결상태에서 $\lambda_p=0.300[W/m{\bullet}k](0\sim-20^{\circ}C)$이고, 동결상태에서 $\lambda_p=0.488[W/m{\bullet}k](-5\sim-20^{\circ}C)$였으며 이들은 실험온도 범위내에서 온도의존성을 나타내지 않았다. 4) 대두단상질의 고유열전도도의 추정치 $\lambda_p=0.300$과 $\lambda_p=0.488$의 타당성을 지질의 함양이 상이한 2종류의 3성분계 두부에 적용한 결과, 실측치와 계산치는 잘 일치했다.