169 research outputs found
ํ๋๋ง Parita Bay์์ 32 ๋ ๊ฐ์ ๋งน๊ทธ๋ก๋ธ ์ฒ ํ ์ง ํผ๋ณต ๋ณํ
ํ์๋
ผ๋ฌธ(์์ฌ)--์์ธ๋ํ๊ต ๋ํ์ :๋์
์๋ช
๊ณผํ๋ํ ์ฐ๋ฆผ๊ณผํ๋ถ(์ฐ๋ฆผํ๊ฒฝํ์ ๊ณต),2019. 8. Kim, Hyun Seok.Mangroves forests around the world have been experiencing a drastic loss. This decrease is attributed in part to changes in bio-climatic factors (e.g. rainfall, temperature, tidal range, extreme events, etc.) and to anthropogenic activities such as coastal development, agriculture, timber extraction, upstream discharge of contaminants, as well as aquaculture and saltpan construction. Whereas remote sensing tools have contributed to detect mangrove vulnerable areas in order to respond with appropriate conservation policies. The principal aims of our study are to quantify the changes in mangrove cover and to identify possible drivers of its change. We present the first mangrove land cover-change analysis in Panama using satellite imagery after the year 2000, and the first in Parita Bay. Mangrove cover changes were determined using Landsat satellite images in four (4) points of time: 1987, 1998, 2009 and 2019, which consequently, were subdivided into three (3) period of study. A supervised classification was employed to quantify changes in areas of different land use-cover types; and the NDVI (Normalized Difference Vegetation Index) was determined for each image, in order to observe changes of greenness in mangrove canopy cover. Our study revealed mangrove area in Parita Bay has increased by 4.7% during the last 32 years and seems to have a good health status reflected in the presence of high NDVI values. However, there was a 1.26% decline of mangrove cover at the first period (1987 to 1998), principally related to the conversion into other types of vegetation and bare soil. During the same period, results also revealed a high expansion of aquaculture and saltpan by 95.88%, and a decline of ~40% in high and very high-density NDVI (>0.46). After the initial decrease of mangrove area, it increased 6% of its extent for the last two decades, and the annual increment rate was even greater for the last decade (0.43%). The increase of mangroves in Parita Bay was mostly due to the conversion from water, other vegetation and bare soil classes. This leads to assume that natural regeneration characteristics coupled with restoration projects developed in the region may had a positive influence over the mangrove cover. In addition, mangroves in protected areas declined at an annual rate of 0.11%, while the unprotected mangroves increased at 0.50% per year during the last period (2009-2019). Our study suggests continuous management of mangrove forests is essential for the areas where the ecosystem vulnerability is high.์ธ๊ณ์ ๋งน๊ทธ๋ก๋ธ ์ฒ์ ๋ํญ์ ์ธ ์์ค์ ๊ฒฝํํ๋ค. ์ด๋ฌํ ๊ฐ์๋ ์๋ฌผ-๊ธฐํ ์ธ์ (์ : ๊ฐ์ฐ, ๊ธฐ์จ, ์กฐ์ ๋ฒ์, ๊ทนํ ํ์ ๋ฑ)์ ๋ณํ์ ์ฐ์ ๊ฐ๋ฐ, ๋์
, ๋ชฉ์ฌ ์ฑ์ทจ, ์ค์ผ ๋ฌผ์ง์ ์๋ฅ ๋ฐฐ์ถ๊ณผ ๊ฐ์ ์ธ์์ ํ๋๋ฟ๋ง ์๋๋ผ ์์ ๋ฐ ์๊ธ์ผ์ ๊ฑด์ค์ด ์์ธ์ด๋ค. ์๊ฒฉ ํ์ฌ ๋๊ตฌ๊ฐ ์ ์ ํ ๋ณด์กด ์ ์ฑ
์ ์๋ตํ๊ธฐ ์ํด ๋งน๊ทธ๋ก๋ธ ์ทจ์ฝ ์ง์ญ์ ํ์งํ๋๋ฐ ๊ธฐ์ฌํ๋ค. ๋ณธ ์ฐ๊ตฌ์ ์ฃผ์ ๋ชฉ์ ์ ๋งน๊ทธ๋ก๋ธ ํผ๋ณต์ ๋ณํ๋ฅผ ์ ๋ํํ๊ณ ๋ณํ์ ๊ฐ๋ฅํ ๊ตฌ๋์ธ์๋ฅผ ๊ท๋ช
ํ๋ ๊ฒ์ด๋ค. ์ฐ๋ฆฌ๋ 2000 ๋
์ดํ์ ์์ฑ ์ด๋ฏธ์ง์ Parita Bay์ ์ฒซ ๋ฒ์งธ ์ฐ๊ตฌ์์์ ์์ฑ ์ด๋ฏธ์ง๋ฅผ ์ฌ์ฉํ์ฌ ํ๋๋ง์์ ๋งน๊ทธ๋ก๋ธ ํ ์ง ํผ๋ณต ๋ณํ์ ์ฒซ ๋ฒ์งธ ๋ถ์์ ์ ์ํ๋ค. ๋งน๊ทธ๋ก๋ธ ์ปค๋ฒ ๋ณ๊ฒฝ์ 1987 ๋
, 1998 ๋
, 2019 ๋
์ ๋ค ๊ฐ์ง ์์ ์์ Landsat ์ธ๊ณต์์ฑ ์ด๋ฏธ์ง๋ฅผ ์ฌ์ฉํ์ฌ ๊ฒฐ์ ๋์์ผ๋ฉฐ, ๊ฒฐ๊ณผ์ ์ผ๋ก ์ธ ๋ฒ์ ์ฐ๊ตฌ ๊ธฐ๊ฐ์ผ๋ก ์ธ๋ถ๋์๋ค. ๊ฐ๋
๋ ๋ถ๋ฅ๋ ๋ค๋ฅธ ํ ์ง ์ด์ฉ ํ์ง ์ ํ์ ์์ญ์์์ ๋ณํ๋ฅผ ์ ๋ํํ๊ธฐ ์ํด ์ฌ์ฉ๋์๋ค. ๋งน๊ทธ๋ก๋ธ ์บ๋
ธํผ ๋ฎ๊ฐ์ ๋
น์ ๋ณํ๋ฅผ ๊ด์ฐฐํ๊ธฐ ์ํด ๊ฐ ์ด๋ฏธ์ง์ ๋ํด NDVI (Normalized Difference Vegetation Index)๋ฅผ ๊ฒฐ์ ํ๋ค. ์ฐ๋ฆฌ์ ์ฐ๊ตฌ์ ๋ฐ๋ฅด๋ฉด Parita Bay์ ๋งน๊ทธ๋ก๋ธ ์ง์ญ์ ์ง๋ 32 ๋
๋์ 4.7 % ์ฆ๊ฐํ์ผ๋ฉฐ ๋์ NDVI ์์น๊ฐ ์กด์ฌํ ๋ ๊ฑด๊ฐ ์ํ๊ฐ ์ํธํ ๊ฒ์ผ๋ก ๋ํ๋ฌ๋ค. ๊ทธ๋ฌ๋ ์ฒซ ๋ฒ์งธ ๊ธฐ๊ฐ (1987 ~ 1998)์๋ ๋งน๊ทธ๋ก๋ธ ํผ๋ณต์ด 1.26 % ๊ฐ์ํ์ผ๋ฉฐ, ์ฃผ๋ก '๋ค๋ฅธ ์ข
๋ฅ์ ์๋ฌผ'๊ณผ '๋งจ๋
ํ ์'์ผ๋ก์ ์ ํ๊ณผ ๊ด๋ จ์ด์๋ค. ๊ฐ์ ๊ธฐ๊ฐ ๋์ ๊ฒฐ๊ณผ๋ ๋ํ 95.88 %์ ๋์ ์์ ๋ฐ ์๊ธ๋ฌผ ํฝ์ฐฝ๊ณผ ๋์ ๊ณ ๋ฐ๋ NDVI (> 0.46)์์ ์ฝ 40 %์ ๊ฐ์๋ฅผ ๋ํ๋ฌ๋ค. ๋งน๊ทธ๋ก๋ธ ์ง์ญ์ ์ด๊ธฐ ๊ฐ์ ์ดํ ์ง๋ 20 ๋
๊ฐ 6 %์ ์ฆ๊ฐ์จ์ ๋ณด์์ผ๋ฉฐ ์ง๋ 10 ๋
๊ฐ 0.43 %์ ์ฆ๊ฐ์จ์ ๋ณด์๋ค. Parita Bay์ ๋งน๊ทธ๋ก๋ธ (mangroves) ์ฆ๊ฐ๋ ์ฃผ๋ก '๋ฌผ', '๋ค๋ฅธ ์๋ฌผ'๋ฐ '๋งจ์ ํ ์'๋ฑ์ผ๋ก ์ธํ ๊ฒ์ด ์๋ค. ์ด๊ฒ์ ์ง์ญ์์ ๊ฐ๋ฐ ๋ ๋ณต์ ํ๋ก์ ํธ์ ๊ฒฐํฉ ๋ ์์ฐ ์ฌ์ ํน์ฑ์ด ๋งน๊ทธ๋ก๋ธ ํผ๋ณต์ ๊ธ์ ์ ์ํฅ์ ์ค ์ ์๋ค๊ณ ๊ฐ์ ํ๋ค. ๋ํ, ๋ณดํธ ์ง์ญ์ ๋งน๊ทธ๋ก๋ธ๋ ์ฐ๊ฐ ๋น์จ๋ก 0.11 %๋ก ๊ฐ์ํ์ผ๋ฉฐ, ๋ณดํธ๋ฐ์ง ๋ชปํ ๋งน๊ทธ๋ก๋ธ๋ ์ง๋ ๊ธฐ๊ฐ (2009-2019) ๋์ ๋งค๋
0.50 %๋ก ์ฆ๊ฐํ๋ค. ์ฐ๋ฆฌ ์ฐ๊ตฌ๋ ์ํ๊ณ ์ทจ์ฝ์ฑ์ด ๋์ ์ง์ญ์์ ๋งน๊ทธ๋ก๋ธ ์ฒ์ ์ง์์ ์ธ ๊ด๋ฆฌ๊ฐ ํ์์ ์์ ์์ฌํ๋ค.I. Introduction 1
II. Material and Methods 5
1. Study Area 5
2. Data Selection and Image preprocessing 6
3. Image Classification 7
4. Field Ground Truth and Accuracy Assessment 10
5. NDVI Analysis 11
6. Land Cover-Use Change (LUCC) detection 12
7. Analysis in Protected Areas 13
8. Analysis of Environmental variables in the study area 13
III. Results 16
1. Classification Accuracy 16
2. Land Use-Cover Change (LUCC) Detection and mangrove estimation in Parita Bay 18
3. NDVI Classes Changes on time 23
5. Mangroves changes in Protected vs. Unprotected Area 28
6. Local Climatic Variables Analysis 33
6.1 Rainfall 33
6.2 Temperature 34
IV. Conclusion 42
References 44
Web References 50
Appendix A 52
Appendix B 54
Appendix C 55
Appendix D 56
Abstract (in Korean) 57
Acknowledgments 59Maste
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