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闹钟铃声aegean sea有高手能弄出来么
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2。6，选择“重命名”.改好后。3，再选中ituns软件左边列表中的铃声，把改刚才制作好的铃声添加进来.打开“显示简介”后，选择“创建 AAC版本”4，选择“选项”标签，然后把歌曲的播放时间的停止时间改成到40秒那里停，点确定。7。改好后.选中该歌曲右键，把名字后面的m4a改为m4r就行了.“创建AAC版本”后，再选中，右键并选择“在windows管理器中显示”。5.右键选中歌曲铃声1.打开itunes选择左上角的“文件”目录下的“将文件添加到资料库”，这里是打开音乐所在位置，添加音乐到itunes里面，选定要设置的音乐
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求翻译：Aegean丶Sea Team是什么意思？
Aegean丶Sea Team
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爱琴海丶海队
爱琴海丶海队
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Aegean丶Sea 团队
爱琴海？大量的小组
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请输入您需要翻译的文本！From Wikipedia, the free encyclopedia
A map of the Aegean Sea
The extent of the Aegean Sea on a map of the .
The Aegean Sea (; : Αιγα?ο Π?λαγο?  ( ); : Ege Denizi Turkish pronunciation: )[] is an elongated embayment of the
located between the
, i.e., between the mainlands of
and . In the north, the Aegean is connected to the
are within the sea and some bound it on its southern periphery, including
The sea was traditionally known as
(in , Αρχιπ?λαγο?, meaning "chief sea"), but in English the meaning of Archipelago has changed to refer to the Aegean Islands and, generally, to any island group.
In ancient times, there were various explanations for the name Aegean. It was said to have been named after the Greek town of , or after , a queen of the
who died in the sea, or Aigaion, the "sea goat", another name of , one of the archaic , or, especially among the Athenians, , the father of , who drowned himself in the sea when he thought his son had died.
A possible etymology is a derivation from the Greek word α?γε? – aiges = "waves" (; metaphorical use of α?ξ (aix) "goat"), hence "wavy sea", cf. also α?γιαλ?? (aigialos = aiges (waves) + hals (sea)), hence meaning "sea-shore".
The , who ruled many Greek islands in the
and , popularized the name Archipelago ( for "main sea" or "chief sea"), a name that held on in many European countries until the early modern period.
In some South Slavic languages the Aegean is often called White Sea (Belo more/Бело море in Serbo-Croatian and M Бяло море Byalo more in Bulgarian).
The Aegean Sea covers about 214,000 square kilometres (83,000 sq mi) in area, and measures about 610 kilometres (380 mi) longitudinally and 300 kilometres (190 mi) latitudinally. The sea's maximum depth is 3,543 metres (11,624 ft), east of Crete. The
are found within its waters, with the following islands delimiting the sea on the south (generally from west to east): , , , ,
The Aegean Islands, which almost all belong to Greece, can be divided into seven groups:
(or Argo-Saronic Islands)
(or Southern Sporades), with the exclusion of
was originally applied specifically to the Aegean Sea and its islands. Many of the Aegean Islands, or chains of islands, are actually extensions of the mountains on the mainland. One chain extends across the sea to , another extends across
to , and a third extends across the
and Crete to Rhodes, dividing the Aegean from the Mediterranean.
The bays and gulfs of the Aegean beginning at the South and moving clockwise include on Crete, the , ,
bays or gulfs, on the mainland the
to the west with the , the
northwestward, the
which connects with the , the
which connects with the , the
northwestward, the
Peninsula including the
and the , northward the
Gulf, Dikili Gulf, , , , ,
defines the limits of the Aegean Sea as follows:
On the South. A line running from Cape Aspro (28°16'E) in , to Cum Burnù (Capo della Sabbia) the Northeast extreme of the Island of , through the island to Cape , the Southwest point thereof, on to Vrontos Point (35°33'N) in Skarpanto [], through this island to Castello Point, the South extreme thereof, across to Cape Plaka (East extremity of Crete), through Crete to Agria Grabusa, the Northwest extreme thereof, thence to Cape Apolitares in
Island, through the island to Psira Rock (off the Northwest point) and across to Cape Trakhili in
Island, through Kithera to the Northwest point (Cape Karavugia) and thence to Cape Santa Maria () in the .
In the . A line joining Kum Kale (26°11'E) and .
A panoramic view of the , taken from .
A traditional street in Lefkes, -.
Aegean surface water circulates in a counter-clockwise , with
Mediterranean water moving northward along the west coast of , before being displaced by less dense
outflow. The dense
water sinks below the Black Sea inflow to a depth of 23–30 metres (75–98 ft), then flows through the
and into the
at velocities of 5–15 cm/s. The Black Sea outflow moves westward along the northern Aegean Sea, then flows southwards along the east coast of Greece.
The physical oceanography of the Aegean Sea is controlled mainly by the regional climate, the fresh water discharge from major rivers draining southeastern Europe, and the seasonal variations in the Black Sea surface water outflow through the .
Analysis of the Aegean during 1991 and 1992 revealed 3 distinct water masses:
Aegean Sea Surface Water – 40–50 metres (130–160 ft) thick veneer, with summer temperatures of 21–26 °C and winter temperatures ranging from 10 °C (50 °F) in the north to 16 °C (61 °F) in the south.
Aegean Sea Intermediate Water – Aegean Sea Intermediate Water extends from 40–50 m to 200–300 metres (660–980 ft) with temperatures ranging from 11–18 °C.
Aegean Sea Bottom Water – occurring at depths below 500–;m with a very uniform temperature (13–14 °C) and salinity (3.91–3.92%).
A 1528 map of the Aegean Sea by
The current coastline dates back to about 4000 BC. Before that time, at the peak of the
(c. 16,000 BC) sea levels everywhere , and there were large well-watered coastal plains instead of much of the northern Aegean. When they were first occupied, the present-day islands including
with its important
production were probably still connected to the mainland. The present coastal arrangement appeared c. 7000 BC, with post-ice age sea levels continuing to rise for another 3,000 years after that.
The subsequent
civilizations of
and the Aegean Sea have given rise to the general term . In ancient times, the sea was the birthplace of two ancient civilizations – the
of Crete and the
Later arose the city-states of
among many others that constituted the
described the Greeks living round the Aegean "like frogs around a pond". The Aegean Sea was later invaded by the
and the , and inhabited by the , the , the , the , the , and the . The Aegean was the site of the original , and its seaways were the means of contact among several diverse civilizations of the Eastern Mediterranean.[]
Many of the islands in the Aegean have safe harbours and bays. In ancient times, navigation through the sea was easier than travelling across the rough terrain of the Greek mainland (and to some extent the coastal areas of Anatolia). Many of the islands are , and
are mined on other islands. The larger islands have some fertile valleys and plains.
Of the main islands in the Aegean Sea, two belong to  –
( ); the rest belong to . Between the two countries, there are
over several aspects of political control over the Aegean space, including the size of territorial waters, air control and the
of economic rights to the .
Henry George Liddell, Robert Scott, A Greek-English Lexicon, s.v.
Zbornik Matice srpske za dru?tvene nauke: (1961), Volumes 28-31,
(in Serbian)
. Encyclopedia Britannica.
(PDF). International Hydrographic Organization. .
Aksu, A. E., D. Yasar, et al. (1995). "LATE GLACIAL-HOLOCENE PALEOCLIMATIC AND PALEOCEANOGRAPHIC EVOLUTION OF THE AEGEAN SEA – MICROPALEONTOLOGICAL AND STABLE ISOTOPIC EVIDENCE." Marine Micropaleontology 25(1): 1–28.
Yagar, D., 1994. Late glacial-Holocene evolution of the Aegean Sea. Ph.D. Thesis, Inst. Mar. Sci. Technol., Dokuz Eyltil Univ., 329 pp. (Unpubl.)
Tjeerd H. van A Judith C. Shackleton (Winter 1982). . 9,. Journal of Field Archaeology. pp. 445–454.
Tracey Cullen, Aegean Prehistory: A Review (American Journal of Archaeology. Supplement, 1); Oliver Dickinson, The Aegean Bronze Age (Cambridge World Archaeology).
John F. C Despina M Lauren E. Talalay. The familiar phrase giving rise to the title Prehistorians Round the Pond: Reflections on Aegean Prehistory as a Discipline.
Wikimedia Commons has media related to .
Wikivoyage has a travel guide for .
has the text of the
. Foundation of the Hellenic World. Archived from
on 10 August .
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