Tajvanski moreuz

мореуз између Кине и острва Тајван

Tajvanski moreuz (kin. 臺灣海峽) prolaz je koji deli ostrvo Tajvan od kopnene Kine. Moreuz je deo Južnog kineskog mora i povezuje Istočnokinesko more na severu. Najjuži deo moreuza je širok 130 kilometara.[1]

Tajvanski moreuz
Mapa koja pokazuje površinu Tajvanskog moreuza
Koordinate24° 48′ 40″ N 119° 55′ 42″ E / 24.81111° S; 119.92833° I / 24.81111; 119.92833
Okean/moreIstočnokinesko moreJužnokinesko more
Zemlje basenaTzv. Republika Kina (Tajvan)
NR Kina
Maks. dužina360 km
Maks. širina130 km
Maks. dubina1.773 m
OstrvaArhipelag Penhu
Vodena površina na Vikimedijinoj ostavi

Tajvanski moreuz je sam po sebi predmet međunarodnog spora oko njegovog političkog statusa. Pošto Narodna Republika Kina tvrdi da uživa „suverenitet, suverena prava i jurisdikciju nad Tajvanskim moreuzom“ i smatra plovni put „unutrašnjim teritorijalnim vodama“ umesto međunarodnim vodama, to znači da kineska vlada poriče da bilo koje strano plovilo ima slobodu plovidbe u moreuzu.[2][3][4] Ova pozicija je izazvala oštre primedbe Sjedinjenih Država, Australije, Francuske i Tajvana.[5][6][7][8]

Geografija uredi

Tajvanski moreuz je vodeno telo koje odvaja provinciju Fuđen od ostrva Tajvan. Međunarodni sporazum ne definiše Tajvanski moreuz, već stavlja njegove vode unutar Južnog kineskog mora, čija severna granica ide od rta Fugui (najsevernija tačka na ostrvu Tajvan; Fukikaku) do ostrva Niušan do najjužnije tačke ostrva Pingtan i odatle na zapad duž paralelno 25° 24′ S. do obale provincije Fuđen.[9] Nacrt za novo izdanje IHO-ovih Granica okeana i mora precizno definiše Tajvanski moreuz, klasifikujući ga kao deo severnog Tihog okeana.[10] To čini Tajvanski moreuz vodenim telom između Istočnog i Južnog kineskog mora i ograničava ga:[11]

Na severu: linija koja spaja obalu Kine (25° 42′ S - 119° 36′ I) na istok do rta Sjang (25° 40′ S - 119° 47′ 10″ E), severnog kraja ostrva Hajtan, a odatle do rta Fuguj (25° 17′ 45″ S - 121° 32′ 30″ I), severnog kraja ostrva Tajvan (zajednička granica sa Istočnim kineskim morem, videti 7.3).

Na istoku: Od rta Fuguj prema jugu, duž zapadne obale ostrva Tajvan, do rta Eluan (21° 53′ 45″ S - 120° 51′ 30″ I),, južnog kraja ovog ostrva.

Na jugu: linija koja spaja rt Eluan na severozapadu, duž južnih obala ostrva Nanao, do jugoistočnog kraja ovog ostrva (23° 23′ 35″ S - 117° 07′ 15″ I); odatle na zapad, duž južne obale ostrva Nanao, do Čangšan glave (23° 25′ 50″ S - 116° 56′ 25″ I), zapadnog kraja ovog ostrva; a odatle linija koja spaja Čangšan glavu na zapad do ušća reke Hanđang (23° 27′ 30″ N - 116° 52′ E), na obali Kine (zajednička granica sa Južnim kineskim morem, videti 6.1).

Na zapadu: Od ušća reke HanĐang na severoistoku, duž obale Kine, do položaja 25° 42′ S - 119° 36′ I.

Ceo moreuz se nalazi na azijskom kontinentalnom pojasu. Duboka je skoro u potpunosti manje od 150 m (490 ft; 82 fathoms), sa kratkom jarugom te dubine na jugozapadnoj obali Tajvana. Kao takvom, u moreuzu ima mnogo ostrva. Najveća i najvažnija ostrva na obali Fuđena su Sjamen, Gulangju, Pingtan („Hajtan“ po definiciji IHO ), Kinmen i Macu. Prva tri kontroliše Narodna Republika Kina (NRK), a poslednja dva od Republika Kina. Unutar moreuza se nalaze Penghu ili Peskadores, koje takođe kontroliše Tajvan. Postoji velika podvodna obala 40—60 km (25—37 milja) severno od ostrva Penghu.[12]

 
Raspodela reka na Tajvanu i njihovo godišnje opterećenje sedimentom

Srednja linija uredi

Istorijski gledano, i Narodna Republika Kina (NRK) i Republika Kina na Tajvanu su zastupale politiku jedne Kine koja je tesnac smatrala delom ekskluzivne ekonomske zone jedne „Kine“.[13] U praksi, pomorska granica kontrole postoji duž srednje linije niz moreuz.[14] Srednja linija je definisana 1955. od strane generala američkog vazduhoplovstva Bendžamina O. Dejvisa mlađeg koji je povukao liniju niz sredinu moreuza, a zatim su SAD izvršile pritisak na obe strane da uđu u prećutni sporazum da ne prelaze srednju liniju. NRK nije prešla srednju liniju sve do 1999. godine, međutim, nakon prvog nasrtaja 1999. godine, kineski avioni su prelazili preko srednje linije sa sve većom regularnošću.[15] Srednja linija je takođe poznata kao Dejvisova linija.[16]

Geologija uredi

Raspodela sedimenta uredi

Svake godine, tajvanske reke nose do 370 miliona tona sedimenata u more, uključujući 60 do 150 miliona tona deponovanih u Tajvanski moreuz.[17] Tokom proteklih deset hiljada godina, 600 milijardi tona rečnih sedimenata je deponovano u Tajvanskom moreuzu, lokalno formirajući sloj debljine do 40 m u južnom delu Tajvanskog moreuza.[17]

Galerija uredi

Vidi još uredi

Reference uredi

  1. ^ „Geography”. Government Information Office. Arhivirano iz originala 29. 12. 2010. g. Pristupljeno 23. 1. 2011. 
  2. ^ „Foreign Ministry Spokesperson Wang Wenbin's Regular Press Conference on June 13, 2022”. Ministry of Foreign Affairs of the People's Republic of China. 13. 6. 2022. Arhivirano iz originala 6. 8. 2022. g. Pristupljeno 16. 8. 2022. 
  3. ^ Lynn Kuok (13. 7. 2022). „Narrowing the differences between China and the US over the Taiwan Strait”. International Institute for Strategic Studies. Arhivirano iz originala 16. 7. 2022. g. Pristupljeno 16. 8. 2022. 
  4. ^ Jill Goldenziel (28. 6. 2022). „China Claims To Own The Taiwan Strait. That's Illegal.”. Forbes. Pristupljeno 16. 8. 2022. 
  5. ^ „America and China spar over the Taiwan Strait”. The Economist. 23. 6. 2022. Arhivirano iz originala 16. 8. 2022. g. Pristupljeno 16. 8. 2022. 
  6. ^ David Crowe, Peter Hartcher (6. 8. 2022). „Marles accuses China of breaching UN rules with Taiwan exercises”. The Sydney Morning Herald. Arhivirano iz originala 11. 8. 2022. g. Pristupljeno 16. 8. 2022. 
  7. ^ „MOFA solemnly reiterates that the Taiwan Strait constitutes international waters, refuting false claims made by Chinese officials during recent meetings with the US”. Ministry of Foreign Affairs, Republic of China (Taiwan). 14. 6. 2022. Arhivirano iz originala 3. 8. 2022. g. Pristupljeno 16. 8. 2022. 
  8. ^ Yang Cheng-yu, William Hetherington (11. 7. 2022). „Strait belongs to all: top French officer”. Taipei Times. Arhivirano iz originala 13. 7. 2022. g. Pristupljeno 16. 8. 2022. 
  9. ^ IHO (1953), §49.
  10. ^ IHO (1986), Ch. 7.
  11. ^ IHO (1986), Ch. 7.2.
  12. ^ Sea depth map.
  13. ^ Trent, Mercedes (2020). „Over the Line: The Implications of China's ADIZ Intrusions in Northeast Asia” (PDF). Federation of American Scientists. str. 22. Arhivirano (PDF) iz originala 2022-10-09. g. Pristupljeno 4. 8. 2022. 
  14. ^ 大公報文章:"海峽中線"應該廢除, chinareviewnews.com, Arhivirano iz originala 04. 10. 2011. g., Pristupljeno 09. 03. 2023 .
  15. ^ Tai-ho, Lin. „Air defense must be free of political calculation”. www.taipeitimes.com. Taipei Times. Pristupljeno 27. 9. 2020. 
  16. ^ Micallef, Joseph V. (6. 1. 2021). „Why Taiwan Will Be at the Center of the China-US Rivalry”. www.military.com. Military.com. Pristupljeno 10. 1. 2021. 
  17. ^ a b Liu, J. P.; Liu, C. S.; Xu, K. H.; Milliman, J. D.; Chiu, J. K.; Kao, S. J.; Lin, S. W. (20. 12. 2008). „Flux and fate of small mountainous rivers derived sediments into the Taiwan Strait”. Marine Geology (na jeziku: engleski). 256 (1): 65—76. Bibcode:2008MGeol.256...65L. ISSN 0025-3227. doi:10.1016/j.margeo.2008.09.007. 

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