全國高等院校影視專業(yè)委員會年會媒體策劃案

1、 ASSOCIATED MARITIME COMPANY (DA LIAN) LIMITED Passage Plan (Voyage No.1105c) From: Dalian ,China (ZD=-0800) To: San Francisco ,USA (ZD=+0800) ( Safety is always the top priority !)Content index:1) Voyage plan checklist.2) Departure arrival port information.3) Publication in use. 4) Routing weather

2、and currents.5) Other important informations and Special instructions.6) Environment Protection For Passage.7) Contingency Planning.8) Voyage plan and route information.9) Ships Squat.10) Tidal information.25PILOT CARD Ships name YUAN SHAN HU Date _ July 18th 2012_Call sign BOGF Deadweight 297,305 t

3、on Tear built 2010 Draft Molded Aft_m Forward_m Displacement_m SHIPS PARTICULARSLength overall max: 330.00m Anchor chain: Port 14 shackles, Starboard 14 shacklesBreadth: 60.67m (1 shackles=27.5m)Bulbous bow Yes/No 330m29.7m65.53m279.65m50.35m60.67m STEERING PARTICULARSType of rudder the streamline f

4、ormed,double plated, Semi-balanced typeMaximum rudder angle 35Time hard-over to hand-over with two power unit 269(sec)CHECKED IF ABOARD AND READYAnchors Steering gear Whistle Number of power Radar 3 cm 10 cm units operating ARPA Indicators:Russer Speed log Doppler yes no Rpm/Pitch Water speed Rate o

5、f turn Ground speed Compass system Dual-axis constant gyro error Engine telegraphs VHF Elec.pos.Fix.System Type GPS JRC JLR.7700 MK. 1)Voyage Planning ChecklistVessel name : M.T"NEW PARADISE Voyage No.: 1105C Date: December 22th 2012 Master's name: Capt. Kim Jin Hyo From: Vancouver To: Shan

6、ghai AIn preparing the attached voyage plan. the follow publications were Sailing directions/U.S Course PilotTide TablesRadio Navigational AidsNotice to MarinersTide Current TablesOther Ship's routingLocal VTS Light Listother Above publication were catch corrected through Notice to Mariners Numb

7、er STM No. No.37 2012 NONE was not correctedBVessel tracklines are land out on chart number SEE VOYAGE PLAN IN DETAILS Above chart were catch corrected through Notice to Mariners Number: STM No. No.37 2012 CRadio electronic broadcasts consulted:Local Broadcast Notice to MarinersNAVTEXweather RadioIN

8、MARSATWeather Facsimileother DPilot will be contactedTug escort(s)will be contactedEThe vessel's destination berth/anchorage is San Francisco ,USA Depth of water will be at low waterVessel's draft is: 19.8 m forward, 19.8 m aft. Tidal range is N/A FThe following standard emergency procedures

9、 have been reviewed:FireSteering FailureMedical EvacuationCollisionEngine FailureMan OverboardGroundingPollution IncidentElectrical FailureGThe Chief Engineer has been consulted regarding the following:Pre-arrival Tests and InspectionsInoperable/Malfunctioning SystemsStability ConsiderationsOn-going

10、 Maintenance ItemsBallast ConsiderationsOthersHThe following Navigation Officer and Bridge Team Members have been briefed on this Voyage plan: MASTER CHIEF OFFICER SECOND OFFICER THIRD OFFICER THIRD OFFICER THIRD OFFICER (Masters signature) (Date) 2.Departure and arrival port information1. Departure

11、 port: DA LIAN.CHINA2.Arrival port : SAN FRANCISCO ,USA 3.Publication in use (including BA chart)1.Navigation charts in use :3637-1255-1254-4509-2347-4053-4050-2292.Planing charts: 40083.General charts: 4053 40504.Routing charts: 5126(07) 5127(07)5.Plotting sheet: Nil6.Marine routing guide: Ships Ro

12、uting7.Guide to tanker port: Dalian ,China &San Francisco ,USA8.Sailing directions: NP 32 NP 42A NP 41 NP 25 9.ALRS: NP 281(2) NP 282 NP 283(2) NP 284 NP 285 NP 286(5) 10.Admiralty light lists: NP 7911.Tidal tables: TIDE TABLES(BOHAI SEA AND YELLOW SEA) NP 204-0212. NP 136 Ocean passage for the

13、world13. NP 131 Catalogue of ADMIRALTY CHARTS AND PUBLICATIONS 4.Routing weather and currentsRouting currentsl Currents in Huang HaiFrom the limited number of observations available,the currents are frequently weak and variable in the central area with a mainly weak S-setting current in the W and we

14、aker N-setting current in the E. However the constancy of both of these currents is very low and with an average rate of 1/4 kn or less though on some occasions rates of 3 kn have been recorded.(Refer to NP32 Page 26)l Japan CurrentJapan Current has similarities to the Gulf stream of the N Atlantic,

15、being a strong,narrow,warm current of high constancy and forming the NW part of a rather complex clockwise circulation of the N Pacific. The W-setting current, in the S part of this clockwise pattern is known as the North Equatorial Current. This current is blocked to the W by the Philippine islands

16、 and so divides into a S-setting current and a N-setting current towards Taiwan.As the water flow converged to the SE of Taiwan and sets NE,it becomes Japan Current. It becomes somewhat wider with a slightly lower average rate sd it crosses the SE part of Dong Hai,then sets ENE to the S of Japan(Ref

17、er to NP32 Page 26 )l Counter currents SE of the Japan Current.There are probably counter-currents of limited extent on the Pacific side of the Japan Current but information is sparse.Such counter-currents have been observed off the section of the current that passes Taiwan and also SE of Tokara Kai

18、kyo.(Refer to NP42A Page 24)l Pacific CurrentsOver much of the area covered by this book the currents are influenced by the SE and NE Trade Winds of the S and N hemispheres, respectively. These winds induce generally W setting currents across the central Pacific Ocean with little seasonal variation;

19、 principal among these are the South Equatorial Current and North Equatorial Current with a narrow zone of currents setting E between them, as shown on diagrams.(Refer to NP 62 Page 34)l California CurrentThe North Pacific current usually swings S on meeting the American coast to form the California

20、 Current.The California Current has an average rate of ½ kn or less but may increase to about 1 kn at times,particularly in the N of the area.In the area of the California Current,prevailing NW winds give rise to cold water upwelling areas along the North American coast from spring to late summ

21、er.(Refer to NP8 Page 23)Routing weatherEast China sea l Sea surface temperatureDiagrams 1.141.1 to 1.141.4 show the mean sea surface temperatures for February, may,August. The seasonal range is greatest in the N and NW winds from the Asian continent bring the sea surface temperatures down to near o

22、r below freezing in winter. In summer the ean sea temperature is about 23 to 26。Even over the N part of Taiwan Strait there is considerable seasonal variation of between 14 and 16 in February to between 27 and 28 in August. (Refer to NP32 Page 26)l Sea condition 1.Sea waves generated by wind can var

23、y greatly in direction particularly during the transitional months between the NE and SW monsoons. Sea waves are generally lower than expected in the bays and inlets of Bo Hai and Huang Hai due to shorter fetches.2.During the NE monsoon from October to March,waves are mainly from NNW IN Bo Hai and H

24、uang Hai .NNE over S Dong Hai and predominantly NE towards Taiwan. Between June and August ,during the SW monsoon,sea waves are predominantly from the S over Huang Hai and N Dong Hai ,SSW over S Dong Hai and SW to the S of Taiwan strait. (Refer to NP32 Page 26)South east coast of Japanl Sea temperat

25、ureThe sea temperature is relatively high throughout the year due mainly to the influence of the Japan Current which flows along the S coasts of Japan.The sea is warmest in August and coldest in February;see Diagrams 9 to 12.The decrease in temperature from S to N is substantial excepe in August whe

26、n there is comparatively little variation.Abnormal temperature are likely when the seasonal monsoons are particularly dominant and prolonged.(Refer to 42A page24) l Winds and galesLand and sea breezes are a regular feature in settled weather from May to September .These diurnal changes are evident i

27、n the wind summaries given in the Climatic Tables(1.97 to 1.118).The seasonal percentage of winds of force 7 to over is shown on Diagrams 25 and 26 and in the Climatic Tables.The majority of strong winds and gales develop around the perimeter of depressions an they pass E or NE over the area,or are

28、associated with tropical revolving storms.(Refer to 42A page 43)l Fog and visibility.Fog is rare at sea during the months when the N monsoon predominates. From September to April the average frequency of fog is the everywhere blow 2 percent and for much of the winter the frequency increases to about

29、 3-4 per cent. Patches of fog may occur with S winds in advance of a depression.In summer air of tropical origin becomes very humid as S winds carry it towards the S coasts of the main islands and sea fog may be formed.(Refer to 42A page 44)Pacific oceanl Pressure Average distribution e distribution

30、 at MSL in January, April, July and September is shown in diagrams to 1.147.1 to 1.147.4 and illustrate the typical mean pressure fields for the NE and SW monsoons. The pressure pattern is dominated by the Siberian anticyclone in winter creating strong N-NE monsoon winds due to intense pressure grad

31、ients. The collapse of the anticyclone in spring results in reduced pressure gradients over the area. In summer low pressure covers Asia and the W Pacific anticyclone extends W, giving rise to relatively weak S and SW winds. In September the Siberian anticyclone starts to build once more causing the

32、 return of N to NW monsoon winds.(Refer to NP 32 Page 34)l Tropical cyclonesThese storms are more frequent over the W part of North Pacific Ocean than in any other part of the word, with an average of about 25 to 30 per year. The majority form over the islands of Guam and Yap in the Pacific E of the

33、 Philippines archipelago. Tropical storm or typhoons may occur in any month but are rare in winter and spring. Of those that do from about half recurve N-wards as they approach the archipelago. In Bo Hai and Liaodong there is seldom more than one tropical storm affecting the area each year and this

34、usually occurs during July or August.(Refer to NP 32 Page 34)l Fog and visibilitySea fog is rare within the limits of the book between August and January, the frequency being less than 2%. Most sea fogs occur between March and July with greatest frequency during May when occurrences are 10 to 15% ov

35、er the coastal waters between Shanghai and Qingdao thence steadily decreasing to less than 2% In Taiwan Strait. See diagram 1.167.(Refer to NP 32 Page 48)l PressureDiagrams show the mean barometric pressure distribution for January, April, July and South Pacific Ocean with an intervening low pressur

36、e belt appear on all monthly mean pressure charts throughout the year although they vary in intensity and position with the seasons, following the apparent movements of the sun. The anticyclones are farthest N in the N summer and farthest S during the N winter.(refer to NP 62 Page 44)l WindsThe diag

37、rams giving the mean pressure distributions also show the dominant winds for the same months; the arrows fly with wind. In some places the most dominant wind is only marginally more frequent than the winds in adjacent quadrants.Winds with a W component are the most frequent N of 40°N throughout

38、 the year and during the winter they encroach as far S as 30°N. They are usually strongest in winter but can reach gale force at times in summer also.(refer to NP 62 Page 45)Pacific coasts of Central America l Sea surface temperature The mean sea surface temperatures for January and July are sh

39、own in diagram 1.169.Sea surface temperatures are generally at their lowest in late January a d February and highest in August.Mean sea surface temperatures remain around 26 in the S of the area throughout the year,and with temperatures increasing from 6°to 12 in the extreme NW of the area betw

40、een January and July .The effect of the cold California Current on the sea surface temperature isotherms is well marked,particularly in summer,and extends S from about 45°N to 20°N.There is also considerable upwelling of cold water in the vicinity of this current which is favourable for fo

41、g formation with warm moist W to NW winds.l WindsOn the E flank of the North Pacific anticyclone,N to NW winds extends from around 25°N to32°N over the open sea (and to about 40°N in coastal areas) in the winter ,and to near 50°N in summer.The North-east Trade Winds blow on the S

42、 side of the anticyclone and extend S from about 25°N in winter ,and 30°N in summer ,to near the equatorial trough .Winds are moderate ,generally around force 3 to 5 but with some increase in strength in the winter months ,especially in the W of the area ,These winds tend to back N or NW n

43、ear the coast which results in a mainly N to NW flow along the whole coastline from 15°to around 40°N in winter and near 50°N in summer .l Fog and visibilityThe greatest frequency of fog occurs off the coast of California between 36°and 40°N where between 10 and 20 per cent

44、of all observations record fog in all months expect for April ,May and November .Sea fog is most widespread between July and October ,and during September frequently extends N to Cape Flattery .In most seasons the fog frequency decreases with increasing distance form the coast ,especially to the S o

45、f about 32°N ，however ，off the coast of Washington , in August ,around 10 to 20 per cent of observations record fog out to around 140°W .Other important information and special instructions South east coast of Japanl Caution Although warning of he position,intensity and expected movement o

46、f a typhoon is broadcast at frequent intervals,sometimes there is insufficient evidence for an accurate warning,or even a general warning,to be given and vessels must be guided by their own observations.The corrected barometer reading of 3 mb or more below the mean for the time of year,is far the mo

47、st reliable indication of the proximity of a storm.(Refer to 42A page 43)Pacific oceanl TidesIn the island groups described in this volume the tides are predominantly semi-diurnal, except for the Hawaiian Islands, including the small islands extending WNW from the main islands, where the tides have

48、a strong diurnal inequality.In most place the range of the tide is from 0.5m to1.0m. The greatest range, of 1.1m, is found in Marquises and the smallest, of 0.3m, in Northern Cook Islands.(refer to NP 62 Page 34)l CautionThe Climatic tables give meteorological data for a number of land stations whic