• 대한원격탐사학회지
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• 제29권1호
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• pp.1-9
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• 2013

그린란드 북쪽 정착빙 부근 해빙을 분류하기 위하여 현장 자료, 다중 주파수 SAR (Synthetic Aperture Radar) 영상, 텍스쳐 영상을 사용하였다. 해빙의 유형은 first year ice, highly deformed ice, ridge, moderately deformed ice 총 4개로 분류하였다. K-means 알고리즘을 사용하여 텍스쳐 영상으로 분류한 경우 SAR 영상을 사용했을 때 보다 전체 정확도가 높게 나타났으나, 최대 우도법(maximum likelihood) 알고리즘을 사용하였을 때 텍스쳐 영상의 전체 정확도는 때에 따라서 높게 나타났다. 단일 영상 및 다중 영상을 사용했을 때 결과를 비교하면, K-means 알고리즘을 사용했을 때는 다중 영상을 이용하는 것이 전체 정확도가 높게 나타났다. 최대 우도법 알고리즘을 사용했을 경우, 단일 영상을 사용했을 때와 다중 영상을 사용했을 때 클래스별 분류 정확도가 차이가 있어 단일 영상과 다중 영상을 적절하게 사용해야 한다고 판단된다.

• 대한원격탐사학회지
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• 제40권3호
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• pp.285-293
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• 2024

본 연구는 Google Earth Engine을 활용하여 Sentinel-1 Synthetic Aperture Radar 영상을 통해 남극 Campbell Glacier Tongue (CGT)와 Drygalski Ice Tongue (DIT)의 면적 변화를 2016년부터 2024년까지 모니터링하였다. Otsu 기법과 Simple Non-Iterative Clustering (SNIC) 클러스터링 기법을 사용하여 빙설과 해양을 구분하고 월평균 영상을 통해 빙설 탐지 오류를 줄였다. 분석 결과 CGT는 주기적인 붕괴로 인하여 약 26% 감소하였고 DIT는 전반적으로 증가하다가 최근 급격한 감소를 보였다. Sentinel-2 광학 영상과 비교한 결과 높은 탐지 정확성을 보여 제안된 방법의 신뢰성을 입증하였으며, 본 연구는 남극 빙설과 빙붕의 장기 모니터링에 기여할 것으로 기대된다.

• International Journal of Naval Architecture and Ocean Engineering
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• 제12권1호
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• pp.957-966
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• 2020

This paper presents the virtual mass method to implement the prediction of total resistance for ice-going ship in floe ice region based on the combined method of CFD and DEM. Two ways of floe ice distribution are adopted for the analysis and comparison. The synthetic ice model test has been conducted to determine the optimal virtual mass coefficients for the two different floe ice distributions. Moreover, the further verification and prediction are developed in different ice conditions. The results show that, the fixed and random distributions in numerical method can simulate the interaction of ship and ice vividly, the trend of total resistance varying with the speed and ice concentration obtained by the numerical simulation is consistent with the model test. The random distribution of floe ice has higher similarity and better accuracy than fixed distribution.

• 대한원격탐사학회지
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• 제39권3호
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• pp.257-268
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• 2023

해빙은 지구의 태양에너지 흡수량 및 대기-해양간 열과 물질 교환을 조절함으로써 기후조절자의 역할을 하며 그 생성, 이동, 소멸은 인공위성에 의해 주기적으로 모니터링 되고 있다. 그러나 수동마이크로파방사계 관측을 중심으로 한 저해상 산출물은 해빙 표면이 빠르게 변하는 여름철에 정확도가 크게 떨어지며, synthetic aperture radar (SAR) 관측이 대체재로 떠오르고 있으나 그간의 연구는 주로 겨울철 해빙을 대상으로 이루어졌다. 이 연구에서는 SAR 영상과 global positioning system (GPS) 추적기를 이용하여 해빙의 거칠기, 높낮이, 구조 등 표면 상태 변화가 심한 늦여름~초가을 시기의 해빙 이동 추적 기술을 평가, 분석하였다. 그 결과 겨울철보다는 관측 불확실성이 증가하나 GPS 실측치와의 상관관계는 0.98로 우수했으며, 해빙 농도 50% 이상인 경우에 해빙 농도와 적용 알고리즘의 산출 성능은 상관관계 0.59로 서로 비례하는 것으로 나타났다.

• Journal of Advanced Research in Ocean Engineering
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• 제2권2호
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• pp.67-80
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• 2016

The resistance performance of an icebreaking cargo vessel with varied stem angles is investigated numerically and experimentally. Ship-ice interaction loads are numerically calculated based on the fluid structure interaction (FSI) method using the commercial FE package LS-DYNA. Test results obtained from model testing with synthetic ice at the Pusan National University towing tank and with refrigerated ice at the National Research Council's (NRC) ice tank are used to validate and benchmark the numerical simulations. The designed icebreaking cargo vessel with three stem angles ($20^{\circ}$, $25^{\circ}$, and $30^{\circ}$) is used as the target ship for three concentrations (90%, 80%, and 60%) of pack ice conditions. The comparisons between numerical and experimental results are shown and our main conclusions are given.

• 한국항해항만학회:학술대회논문집
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• 한국항해항만학회 2015년도 추계학술대회
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• pp.33-34
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• 2015

북극항로(NSR)를 통항하는 상선과 화물량이 매년 중가추세에 있다. 쇄빙선의 도움을 받아 북극항로를 통항하는 상선의 안전한 항해를 위협하는 가장 큰 요인은 얼음과의 충돌이다. 따라서 선박과 얼음의 충돌 메커니즘을 규명하기 위한 노력이 관련 연구자들에 의해서 활발히 이루어지고 있다. 본 연구에서는 북극항로를 운항하는 내빙선과 유빙의 충돌을 가정한 예인수조실험을 실시하며, 충돌 후 얼음의 운동(속력, 궤적)을 머신비전검사를 통해서 계측한다. 아울러 오차계산을 통해서 머신비전검사 기법의 정밀도를 검증한다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.892-895
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• 2006

The atmospheric effects on the retrieval of sea ice concentration from passive microwave sensors are examined using simulated data typical for the Arctic summer. The simulation includes atmospheric contributions of cloud liquid water and water vapor and surface wind on surface emissivity on the microwave signatures. A plane parallel radiative transfer model is used to compute brightness temperatures at SSM/I frequencies over surfaces that contain open water, first-year (FY) ice and multi-year (MY) ice and their combinations. Synthetic retrievals in this study use the NASA Team (NT) algorithm for the estimation of sea ice concentrations. This study shows that if the satellite sensor’s field of view is filled with only FY ice the retrieval is not much affected by the atmospheric conditions due to the high contrast between emission signals from FY ice surface and the signals from the atmosphere. Pure MY ice concentration is generally underestimated due to the low MY ice surface emissivity that results in the enhancement of emission signals from the atmospheric parameters. Simulation results in marginal ice areas also show that the atmospheric and surface effects tend to degrade the accuracy at low sea ice concentration. FY ice concentration is overestimated and MY ice concentration is underestimated in the presence of atmospheric water and surface wind at low ice concentration. In particular, our results suggest that strong surface wind is more important than atmospheric water in contributing to the retrieval errors of total ice concentrations over marginal ice zones.

• 천문학회보
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• 제46권1호
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• pp.43.1-43.1
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• 2021

In this study, we suggest a new method to estimate the mass of a halo coronal mass ejection (CME) using synthetic CMEs. For this, we generate synthetic CMEs based on two assumptions: (1) the CME structure is a full ice-cream cone, (2) the CME electron density follows a power-law distribution (ρ_cme=ρ₀r^-n). The power-law exponent n is obtained by minimizing the root mean square error between the electron number density distributions of an observed CME and the corresponding synthetic CME at a position angle of the CME leading edge. By applying this methodology to 57 halo CMEs, we estimate two kinds of synthetic CME mass. One is a synthetic CME mass which considers only the observed CME region (M_cme1), the other is a synthetic CME mass which includes both the observed CME region and the occulted area larger than 4 solar radii (M_cme2). From these two cases, we derive conversion factors which are the ratio of a synthetic CME mass to an observed CME mass. The conversion factor for M_cme1 ranges from 1.4 to 3.0 and its average is 2.0. For M_cme2, the factor ranges from 1.8 to 5.0 with the average of 3.0. These results imply that the observed halo CME mass can be underestimated by about 2 times when we consider the observed CME region, and about 3 times when we consider the region including the occulted area. Interestingly these conversion factors have a very strong negative correlation with angular widths of halo CMEs.We also compare the results with the CME mass estimated from STEREO observations.

• Ocean and Polar Research
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• 제33권1호
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• pp.1-11
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• 2011

This study describes measurements of fast ice recorded on May 23, 2009, in Kongsfjorden (translated as 'Kongs Fjord'), an inlet on the west coast of Spitsbergen in the Svalbard Archipelago. Seasonal fast ice is an important feature for Svalbard fjords, both in relation to their physical environment and also the local ecosystem, since it grows seaward from the coast and remains in place throughout the winter. Ice thickness, snow, ice properties, and wind speed were measured, while SAR (Synthetic Aperture Radar) data was observed simultaneously observed two times from ALOS-PALSAR (L-band). Measured ice thickness was about 25-35 cm while the thickness of ice floe broken from fast ice was measured as 10-15 cm. Average salinity was 1.9-2.0 ppt during the melting period. Polarimetric data was used to extract H/A/alpha-angle parameters of fast ice, ice floe, snow and glacier, which was classified into 18 classes based on these parameters. It was established that the area of fast ice represents surface scattering which indicates low and medium entropy surface scatters such as Bragg and random surfaces, while fast ice covered with snow belongs to a zone of low entropy surface scattering similar to snow-covered land surfaces. The results of this study will contribute to various interpretations of interrelationships between H/A/alpha parameters and the wave scattering Phenomenon of sea ice.

• 대한원격탐사학회지
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• 제34권1호
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• pp.17-24
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• 2018

Grounding line of a glacier or ice shelf where ice bottom meets the ocean is sensitive to changes in the polar environment. Recent rapid changes of grounding lines have been observed especially in southwestern Antarctica due to global warming. In this study, ERS-1/2 and Sentinel-1A Synthetic Aperture Radar (SAR) image were interferometrically acquired in 1996 and 2015, respectively, to monitor the movement of the grounding line in the western part of Ronne Ice Shelf near the Antarctic peninsula. Double-Differential Interferometric SAR (DDInSAR) technique was applied to remove gravitational flow signal to detect grounding line from the interferometric phase due to the vertical displacement of the tide. The result showed that ERS-1/2 grounding lines are almost consistent with those from Rignot et al. (2011) which used the similar dataset, confirming the credibility of the data processing. The comparison of ERS-1/2 and Sentinle-1A DDInSAR images showed a grounding line retreat of $1.0{\pm}0.1km$ from 1996 to 2015. It is also proved that the grounding lines based on the 2004 MODIS Mosaic of Antarctica (MOA) images and digital elevation model searching for ice plain near coastal area (Scambos et al., 2017), is not accurate enough especially where there is a ice plain with no tidal motion.