• Title/Summary/Keyword: Halla Mountain

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Why is Seogwipo Warm in Winter? The wind from Jeju City to Seogwipo-The Wind from Seogwipo to Jeju City (서귀포는 겨울철에 왜 따뜻할까? 제귀지풍과 귀제지풍)

  • Sung kook Lee;Moon Ho Lee;Jeong Su Kim
    • The Journal of the Convergence on Culture Technology
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    • v.9 no.4
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    • pp.121-125
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    • 2023
  • In winter, Jeju's Seogwipo and Jungmun areas are 2~3℃ warmer than Jeju City. The reason is that when the north wind over Halla Mountain crosses Baengnokdam of Halla Mountain and passes the 300m long and 260m vertical rock face of Donnaeko at an altitude of 1600m above sea level, the cold air turns into warm air through adiabatic compression, and the warmth rides on Donnaeko and flies to Seogwipo and Jungmun. Conversely, the south wind that rises over the sea in Seogwipo in the summer passes over Hallasan Mountain and passes 99 valleys before turning into a muggy, humid climate, making Jeju hot. In other words, it is because of The wind from Jeju City to Seogwipo-The Wind from Seogwipo to Jeju City.

Spatial and Temporal Analysis of the Coleopteran Communities around 5.16 Road of Mt. Halla, Jeju Island, Korea (한라산 5.16 도로변에 분포하는 딱정벌레류(類)의 월별과 고도별 군집 분석)

  • Yang, Kyoung-Sik;Kim, Sang-Bum;Kim, Won-Taek
    • Korean Journal of Environmental Biology
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    • v.24 no.4
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    • pp.337-358
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    • 2006
  • The field survey was conducted weekly from April to October in 2004 and 2005 on the sites along the 5.16 road. Sampling sites were made every 100 m height starting from 250 m altitude of both sides of Mt. Halla along 5.16 Road, which crosses the mountain from North to South. Totally 31,698 individuals of 76 species belonged to 25 families were collected. It was July that showed the largest number of species, as 48 species in the northern sloper 42 in the southern slope, and 22 at the highest site (at an altitude of 750 m), while it was April that showed the smallest as 17 species, 15 and 5, respectively. As for monthly fluctuation, the northern slope and the highest site reached their top in August, whereas it was June in the southern slope. In the analyses of similarity (chord distance) of any pair of temporal communities, the closest pair was between June and July in the northern slope area, between July and August in the southern slope and between July and September at the highest site, respectively.

Native Cornus kousa Community and Its Habitat in Jeju Island (제주도 산딸나무 군락의 생태적 특성)

  • 안영희;심경구
    • Journal of Environmental Science International
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    • v.12 no.1
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    • pp.15-22
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    • 2003
  • Fifteen major naturally populated habitats around the Mt. Halla, Jeju province for wild Cornus kousa are mostly located on the southeast side of the mountains at 850-1,550m in altitude at sea level and are in half sunney areas. More than 40.0% of the naturally populated area of Cornus kousa are edge of forest areas and 53.3% populate on the steep slope of the mountain in 0-5℃. The direction of the slop for about 40.0% of total populated areas is southeast. In the naturally populated areas, total of 64 taxa dividing into 42 families, 59 genera 56 species and 8 varieties have been shown, mostly Hydrangea petiolaris, Rubus oldhamii, Ilex crenata, Sasa quelpaertensis, Ligustrum obtusifolium. It is suggested that these areas are secondary forest in a typical deciduous forest in Mt. Halla where the second transition had been progressed after forest damage or environmental stress. The index of species diversity of plant groups in these areas is 1.286-4.238 based on the Shannon-Wiener's method.

Rock-Surface Temperatures of the Summit Area of Mt. Halla as a Habitat for an Arctic-alpine Plant Diapensia lapponica var. obovata (돌매화나무 서식지로서 한라산 정상 암벽 표면의 온도특성)

  • Kim, Taeho;Lee, Seung-Wook
    • Journal of The Geomorphological Association of Korea
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    • v.25 no.4
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    • pp.89-101
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    • 2018
  • In Mt. Halla, an arctic-alpine plant Diapensia lapponica var. obovata largely clings to rock surfaces. We observed the rock-surface temperatures of a rocky ridge on the summit area of the mountain from late April 2009 to early May 2010 in order to examine the diurnal and annual temperature variations and the thermal amplitude. We also investigated temperature regimes such as the frequency of freeze-thaw cycles and the temperature change, which might endanger the habitat through frost weathering. For comparison of slope aspects, temperature monitoring was carried out on the north and south faces of the same rocky ridge. The south face experiences the high daily maximum rock-surface temperatures and the high thermal amplitudes during the unfreezing season of May to November 2009. The temperature regimes are considered to exert physiological stress to the arctic-alpine plant. In addition, the south face shows the high frequency of freeze-thaw cycles during the seasonal freezing period of December 2009 to April 2010. This indicates that the south face is susceptible the exfoliation and granular disintegration of rock surfaces, which results in habitat destruction. As a consequence, the south face is believed to be less favorable for the establishment and growth of the arctic-alpine plant than the north face on the summit area of Mt. Halla.

The Land Surface Temperature Distributions of Jeju Island using Landsat 7/ETM+ Data

  • Lee Byung-Gul
    • Journal of the Korean earth science society
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    • v.26 no.2
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    • pp.109-113
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    • 2005
  • In this study, the estimation of the temperature distribution of Jeju Island with coastal ocean derived from the thermal band of Landsat 7/ETM+ of January 6, 2003 was carried out. For the computation of the temperature of the island and the coastal ocean based on the thermal band, we used NASA method wiich is the 8 bit Digital Number(DN) converted into spectral radiance. The computed results showed that the land temperature variations were from 0 to 12 Celsius degrees, and a good agreement with the observation ones based on the method. However, the ocean surface temperature was not much changed ground 15 degree since the water was well mixed between the coastal and the offshore ocean. The interesting results were that the temperature distributions of the southern part(Seogwipo City) of Jeju Island were higher than those of the north one(Jeju City) by more than 2 Celsius degree at the same height although the distance between the Jeju and the Seogwipo is only about 35km in winter season. The reason was found that the solar irradiance intensity of the south part was stronger than the north one by Halla mountain in winter season only. From the results, we found that the seasonal variations of solar irradiation and the height of Mt. Halla were an important role of temperature distribution of Jeju Island.

Cellular Slime Molds of Halla Mountain, III - Description of Polar Granule Positive Species - (한라산의 세포성 점균 (III) - 극낭 양성 종의 기록 -)

  • 홍정수
    • Journal of Plant Biology
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    • v.35 no.4
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    • pp.307-316
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    • 1992
  • A key to the species which have been isolated from the Korean forest soils was provided, and three unrecorded species found in the forest soils of Mt. Halla were described and illustrated. Twenty dictyostelid cellular slime molds had been found in Korean forest soils. Among these, nine species were PG positive, and eleven species were PG negative. Three species described in this study were all PG positive. These were Dictyastelium aurea-stipes Cavender, Raper et Norberg vaL aurea-stipes (new strain HL-5), Dictyastelium monachasiaides Hagiwara, PalysPhandylium tenuissimum Hagiwara. Morphological features and growth habits of these species were examined and compared, and their distribution patterns were illustrated.trated.

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The Halla Seolmundae Inner Body and Soul: From The DNA Silk To The Packing DNA Thin Silk (한라 설문대 속살(內肉)과 혼(魂):생명주(生明紬)에서 세명주(細明紬)로)

  • Kim, Jeong Su;Lee, Sung Kook;Lee, Moon Ho
    • The Journal of the Convergence on Culture Technology
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    • v.8 no.4
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    • pp.219-225
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    • 2022
  • 1950-meter-tall goddess is Seolmundae Grandmother with the head of the 1950m Hallasan Mountain Baengnokdam and the body of the mountain ridgeline. Seolmundae Grandmother in Jeju is a folk belief that has been passed down from generation to generation in Jeju. Unlike inland, Seolmundae Grandmother, which had femininity in the customs of Jeju, which was a matrilineal society, developed into an absolute faith in Jeju, metaphorizing that in some way it was inevitable. Seolmundae Grandmother was the only subject that could mentally solve the biggest problem for Jeju residents, even if they were disconnected from the mainland. In other words, Seolmundae Grandmother was unable to make underwear for Seolmundae Grandmother because it was short of 100 bottles of silk, the god of Hallasan, a huge being and a physical symbol. Therefore, Semyungju Grandmother gave up the bridge connecting the mainland and Jeju. In this paper, focusing on the fact that Mt. Halla, covered with snow in winter, is like a skein of silk thread that we usually use in our daily lives, the etymology of Seolmundae has been changed to Saengmyeongju, - Semyungju, which is a skein of fine silk. As a basis for this, there is a custom of tying a thread of silk in 'Semyungju', a shrine to Semyeongju in Halmangdang, 'Hanmosal' along the coast of Pyoseon-myeon. The silk thread is the core of the Packing DNA gene. The summit of Mt. Halla, Ninety-Nine Valleys, and five hundred generals, found in Seolmundae Grandmother or White Silk, expressed the symbols of Jeju. The Packing DNA gene was found to originate in the Jeongnang

Ecogeographical variations of the vegetative and floral traits of Lilium amabile Palibian

  • Nguyen, Viet Yen;Rai, Rameshwar;Kim, Jong-Hwa;Kim, Ji-Young;Na, Jong-Kuk
    • Journal of Plant Biotechnology
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    • v.48 no.4
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    • pp.236-245
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    • 2021
  • This study aimed to characterize the morphological variations in the vegetative and floral traits of 73 wild Lilium amabile plants from six habitats in Korea. It was observed that L. amabile is distributed nationwide at any altitude from 300 m (Mt Mangdaeam) to 1550 m (Mt Halla). The majority of the natural habitats of L. amabile were found on mountain slopes, and some were found in rugged mountain regions. The down-facing flowers of this species not only had many blotches but also dense trichomes, and the flowering time was found to be from mid-June to mid-July. ANOVA revealed significant variations in vegetative and floral traits among the six habitats, indicating that the environment has substantial influences on the various growth parameters of L. amabile, such as plant height; number of leaves, bracts, papillae, and flowers; leaf angle; and lengths of the anther, longest blotch, and nectary of the petiole. In addition, the vegetative and floral traits were found closely correlated with each other under the direct impact of the environment. These findings will facilitate to find the appropriate environmental conditions for the conservation and development of L. amabile population as future lily-breeding materials.

Hydrochemical Characteristics of Spring Water in Cheju Island (제주도 용천수의 수리화학적 특성)

  • 윤정수;박상운
    • Journal of the Korean Society of Groundwater Environment
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    • v.5 no.2
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    • pp.66-79
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    • 1998
  • This study purposes to elucidate the characteristics of local water quality and the evolutional process of the spring water have been studied with the samples from 55 selected springs, from the coast region to the Baegrogdam, a caldera lake of Halla mountain in Cheju Island. Results of hydrochemical analyses in the 55 spring water show that Gwaneumsa is pollued with high hydrogen concentration, and spring waters from Yusuarmchun, Jangsumul, Dukjisemmul, Sinch'onk'nmul, Youngchunsa, Woonyangchun, Harwontongmul, Dongheamul, Seakdalsengsu, Andukkyekok, Dotimul, Kinmul, Harkangmul and Jungkeummul are polluted by the pollution sources from the surface surrounding ground. Spring waters of Samyang3suwon, Meungbusa, Sernurungmul, Tosanmul, Jungkeummul, Kwakgimul, Aewolharmul, Konemul and Nokgomul are also polluted from the sea water intrusion. The electrical conductivity, pH and the concentration of nitrate nitrogen and bicarbonate increase when the precipitation increases, but the concentration of sodium, chloride and sulphate decrease when the precipitation increases. The concentrations of potassium, magnessium and calcium are nearly independent of the precipitaion. Quality characteristics of spring water show complicated group of spring water through piper's trilinear diagram. The high mountain region consists of groups of sodium or potassium type and bicarbonate type; the middle mountain region consists of groups of sodium or potassium type and no dominant type; the low mountain consists of groups of no dominant type and sulfate or nitrate type; the coast region consists of groups of sodium or potassium type and chloride type or no dominant type. These characteristics indicate that the spring waters are changed from bicarbonate type in the high and middle mountain regions into non-bicarbonate type in the coastal region, as the precipitated waters flow downslope.

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