Musim taufan Pasifik 2010: Perbezaan antara semakan

Kandungan dihapus Kandungan ditambah
Hamba Allah (bincang | sumb.)
Hamba Allah (bincang | sumb.)
k Taufan Conson
Baris 39:
===Jun dan Julai===
Hanya satu sistem lekukan tropika yang terbentuk pada bulan Jun. Pada 2 Jun, JMA mengesan sistem tekanan rendah terbentuk di [[Hainan|Pulau Hainan]].<ref>{{Cite web|url=http://www.webcitation.org/5qENmBBgr|title=JMA WWJP25 Advisory 2010-06-02 00z|date=2 June 2010|publisher=Japan Meteorological Agency|accessdate=12 July 2010}}</ref> 36 jam selepas itu, tekanan rendah tersebut bergerak menuju ke arah timur. Ketika berada {{convert|600|km|mi|abbr=on}} barat laut Manila, Filipina, JMA mengesan ia bertukar menjadi lekukan tropika pada hujung hari 3 Jun.<ref>{{Cite web|url=http://www.webcitation.org/5qENQKF3O|title=JMA WWJP25 Advisory 2010-06-03 18z|date=3 June 2010|author=Staff Writer|publisher=Japan Meteorological Agency|accessdate=17 September 2010}}</ref><ref>{{cite journal|author=Staff Writer|date=22 July 2010|title=RSMC Darwin Tropical Diagnostic Statement June 2010|publisher=Bureau of Meteorology|journal=RSMC Darwin Tropical Diagnostic Statement|volume=29|issue=6|page=3|url=http://reg.bom.gov.au/climate/ntregion/statements/tropical/dtds-201006.pdf| accessdate=26 May 2011 | archiveurl= http://web.archive.org/web/20110706121744/http://reg.bom.gov.au/climate/ntregion/statements/tropical/dtds-201006.pdf| archivedate= 6 July 2011| deadurl= no}}</ref> Lekukan tropika ini terus bergerak ke arah timur laut. JMA tidak lagi memantau lekukan tropika ini menjelang awal 6 Jun.<ref>{{Cite web|url=http://www.webcitation.org/5qGhRhGo8|title=JMA WWJP25 Advisory 2010-06-05 18z|date=5 June 2010|author=Staff Writer|publisher=Japan Meteorological Agency|accessdate=17 September 2010}}</ref><ref>{{Cite web|url=http://www.webcitation.org/5sruSaOaH|title=JMA WWJP25 Advisory 2010-06-06 00z|date=6 June 2010|author=Staff Writer|publisher=Japan Meteorological Agency|accessdate=17 September 2010}}</ref>
 
Taufan Conson pada asalnya merupakan suatu lekukan tropika yang terbentuk pada awal 11 Julai dan kemudiannya diberi nama Conson apabila bertukar menjadi ribut tropika hari kemudiannya.<ref>{{cite web|url=http://www.webcitation.org/5r90u5mEW|title=JMA WWJP25 warning 2010-07-11 06z|date=2010-07-11|publisher=Japan Meteorological Agency|accessdate=2010-07-15}}</ref> Menjelang tengah hari 12 Julai, JMA menaikkan taraf Conson sebagai ribut tropika kencang dengan angin selaju 100&nbsp;km/j (65&nbsp;bsj). Pada waktu 1800 UTC, Conson bertambah kuat setelah mencapai status taufan. Taufan Conson mencapai kekuatan maksimum dengan angin 130 km/j pada awal hari esoknya.<ref>{{cite web|url=http://www.webcitation.org/5r9jLYl4i|title=JMA Tropical Cyclone Advisory 2010-07-12 06z|date=2010-07-12|publisher=Japan Meteorological Agency|accessdate=2010-07-15}}</ref><!-- Comment
During July 13 TROPICAL STORM (TS) 03W (CONSON), LOCATED APPROXIMATELY 70 NM
EAST OF MANILA, PHILIPPINES, HAS TRACKED WESTWARD AT 14 KNOTS OVER
THE PAST SIX HOURS. THE SYSTEM WAS DOWNGRADED TO TS STRENGTH (60
KNOTS) BASED ON THE WEAKENING ORGANIZATION DUE TO INCREASING LAND
INTERACTION AND INCREASING NORTHEASTERLY VERTICAL WIND SHEAR (VWS).
ANIMATED INFRARED SATELLITE IMAGERY DEPICTS DEGRADED OUTFLOW OVER
THE NORTHERN SEMI-CIRCLE, PARTICULARLY THE NORTHEAST QUADRANT WHERE
STRONG NORTHEASTERLY UPPER-LEVEL FLOW HAS PENETRATED INTO THE CORE
OF THE SYSTEM. SUBSEQUENTLY, DEEP CONVECTION HAS SHIFTED PRIMARILY
SOUTHWEST OF THE CENTER AND CONVECTIVE BANDING HAS WEAKENED
SIGNIFICANTLY. A 131029Z AMSU IMAGE HIGHLIGHTS THE DRAMATIC CHANGE
THAT HAS OCCURRED OVER THE PAST 12 HOURS AND SHOWS A PARTIALLY
EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) WITH LIMITED DEEP
CONVECTION PERSISTING OVER THE SOUTHWEST QUADRANT. THE LLCC REMAINS
WELL-DEFINED, HOWEVER, WITH CURVED BANDING EVIDENT OVER THE WESTERN
SEMI-CIRCLE. THERE IS GOOD CONFIDENCE IN THE CURRENT POSITION AND
MOTION BASED ON THE AMSU IMAGE AS WELL AS A 130915Z CORIOLIS IMAGE.
THE CURRENT INTENSITY IS CONSERVATIVELY ASSESSED AT 60 KNOTS BASED
ON THE AVERAGE OF DVORAK ESTIMATES RANGING FROM 45 TO 77 KNOTS. THIS
IS SUPPORTED BY A 130151Z ASCAT 25 KM IMAGE SHOWING A SMALL CORE OF
60 KNOT WINDS.-->
 
=== Rumusan ===