|
Marine Meteorology: Koper -
Capodistria
Port Information
Geographic Location
- Coordinates: 45°33'North
13°44'East
- The Port of Koper, Slovenia
is situated at the head of Koprski Bay, which is entered
between Debeli Point (45°35'N 13°42'E) and Petelinji Point
(45°32'N 13°39'E). The city of Koper (once known as
Capodistria) is located on the southeast coast of Koprski
Bay. Koper is located west of a valley that passes between
mountainous terrain lying east of Debeli Point, and the
mountainous terrain lying south and east of Petelinji Point.
The better known city of Trieste, Italy is located
approximately 6 nmi (11 km) north of Koper.
- Anchorage can be made at
several locations near the western edge of Koprski Bay.
Selection of the anchorage to be used is dependent on wind
direction and speed.
Harbor As Haven
- As of the June 1998 port
visit the Port of Koper was undergoing extensive development
that would enlarge the port facilities and realign the port
configuration. The port is comprised of three basins.
- Basin 1 is the
southernmost of the three, and is used for general cargo
purposes. Seven primary berths are identified around the
perimeter of the basin. A Fleet Landing is established
in Basin 1 whenever U.S. Navy ships are anchored in
Koprski Bay. Pier 1 in Basin 1 is the recommended
location.
- Basin 2 lies just north of
Basin 1. It is used primarily for bulk cargo and as an
oil terminal. All petroleum product tankers go to Basin
2.
- Basin 3 is the
northernmost of the three basins. It has RO-RO
facilities on its eastern end. The south side of the
basin is used primarily for the loading and unloading of
bulk materials, including iron ore and coal.
- The berths in the three
basins are oriented east-west, so onsetting and offsetting
forces of Bora winds are minimized. Under-keel clearances of
3.3 to 6.6 ft (1 to 2 m) are required..
- All anchorages in Koprski
Bay are exposed to winds from west through north. Charted
depths in all locations range from 59 to 66 ft (18 to 20 m).
Local authorities state that holding in Koprski Bay is good,
but Mediterranean Pilot states that holding is not good on a
bottom of soft yellow mud or sand. Mediterranean Pilot
further states that "mariners are advised to consider
carefully weather conditions when anchoring" in Koprski Bay.
- The Port of Koper
experiences frequent Bora wind events. The traditional Bora
is a wind whose source is so cold that when the air reaches
the coast, the dynamic warming caused by subsidence is
insufficient to raise the air temperature to the level
normally experienced. The Bora occurs when cold air
accumulates over the Balkan Peninsula to the extent that it
spills over coastal maintain ranges and "falls" down the
steep slopes to the sea. Due to topography differences, Bora
winds at Koper are not as strong as those experienced at
Trieste. Nevertheless, sustained wind speeds of 54 kt (100
kph) have been observed at the Port. Bora events may last
two to three days. There are two types of Boras, known as
"White (anticyclonic) Bora" and "Black (cyclonic) Bora." The
White Bora results when a strong pressure gradient exists
between a cold high pressure area north of Slovenia and a
low-pressure area over the Mediterranean Sea. The White Bora
is characterized by cold, clear weather. The so-called Black
Bora results when the low-pressure area is located over the
Adriatic Sea resulting in cloudy and rainy weather over
Slovenia. Due to the instability of the cold air mass, winds
in a White Bora are gustier than those in a Black Bora. The
gusts can be more than twice the sustained wind speed. The
direction of the wind from either Bora is approximately 060°
in the entrance channel (30° off the port bow of an incoming
vessel) and in Basin 3, the worst affected area of the port.
The direction becomes somewhat more easterly in the southern
parts of the harbor, including Basins 1 and 2. Bora events
are normally strongest and most frequent during the months
of December through March, but can occur outside that
four-month period. They are uncommon during the summer
season, but weak Boras of short duration may occur. Bora
winds do not normally cause problems for ships in port, but
additional mooring lines are deployed when necessary to keep
a ship safe at her berth. The safest anchorage during a Bora
is located in Koprski Bay just south of Debeli Point.
- Koper is also affected by
other wind events, including Scirocco, Jugo, and Maistral.
Scirocco wind directions vary from southeast to
south-southwest and may last for several days. The winds are
more-or-less perpendicular to the orientation of the
entrance channel and cause control problems for ships
entering or leaving port. Sustained Scirocco winds can raise
seas of 6.6 to 9.8 ft (2 to 3 m) in the open water west of
Koper, but waves in the harbor are fetch limited by the land
mass south of Koprski Bay. Consequently, waves in the harbor
are not a problem. Departing vessels up to 1,500 GWT often
anchor in Piranski Bay approximately 8 nmi west-southwest of
the Port of Koper to wait until Scirocco conditions abate
over the open waters of the Adriatic Sea. When strong
southerly Scirocco winds prevail, a location just northeast
of Petelinji Point is recommended as an anchorage at Koper.
- Jugo winds are
southwesterlies, and also pose control problems for ships in
the entrance channel. A location in Koprski Bay
approximately midway between Debeli Point and Petelinji
Point is the preferred anchorage during southwesterly Jugo
winds.
- Maistral is a seasonal
northwesterly wind that is prominent during the months of
May through September. The Maistral commonly occurs between
late morning and 5 or 6 pm, the normal hours of a sea
breeze. Maistral wind speeds are usually in the 11-16 kt
range.
- Local forecasting rules:
- Bora winds will onset
approximately 3-4 hours after "cap clouds" develop over
the mountains east of Koper.
- A Scirocco is forthcoming
if the water level in the harbor is higher than normal.
- A change in weather can be
expected if the Maistral is not blowing by 1000L.
- Forecast availability:
- The Hydrometeorological
Institute of Slovenia maintains a web page on the
Internet for dissemination of weather forecast
information. At the time of this writing, everything is
displayed in Slovenian. However, an English language
version is under development, with completion
anticipated in 1999. The URL for the Hydrometeorological
site is: https://www.rzs-hm.si
Planned content for the
Internet site includes:
24 and 48 hour graphical forecasts for Slovenia and
surrounding territory
Graphical-textual English forecast for maritime regions
Products of LAM (approximately 800 x 800 km, resolution
approximately 10 km)
Precipitation fields (+48 hours, every 6 hours)
Surface wind fields (+48 hours, every 6 hours)
850hPa wind fields (+48 hours, every 6 hours)
Cloudiness (+48 hours, every 6 hours)
Surface wind fields (for maritime region, resolution
approximately 2.5 km)
Alphanumerical observations from surface stations
(synoptic and automatic)
- The above information is
already available on the Internet site, but only in
Slovenian.
- If specific forecast
information is required before the English language version
is available on the Internet, faxed forecasts can be
requested from the Hydrometeorological Institute at
telephone number ++386 61 327 461 (ask for forecasters). A
direct number for obtaining telephone consultations with an
operational forecaster may also be obtained by calling the
aforementioned number.
Currents and Tides
- There is a large
counterclockwise current gyre in the center of the Adriatic
Sea. The large gyre sometimes breaks into two smaller gyres.
In both scenarios, the general current flow is northward
along the eastern shores of the Adriatic Sea and southward
along the western shores.
- A north-setting current with
a maximum speed of approximately 1 kt may be observed along
the coastal waters west of Koprski Bay. In Basin 2 of the
Port of Koper, precipitation runoff at the mouth of the
Rizana River may generate westerly flowing currents of 6 to
7 kt during periods of heavy rain.
- Tidal fluctuation in Koprski
Bay and the Port of Koper is approximately 3 ft (90 cm).
Visibility
- Visibility is generally good
at Koper. During a white Bora, the winds bring dry, clean
air that can persist for days at a time.
- Koper is not far from major
sources of fog, including the Po Valley and the Gulf of
Venice. It is not uncommon for westerly winds to advect fog
from either area to Koper. On average, fog occurs on five to
10 days per year at Koper, with December having more foggy
days than other months.
- During periods of reduced
visibility, a ship may not depart the harbor until
visibility improves to at least twice the vessel's length.
Hazardous
Conditions
Spring
- The spring season over the
northern Adriatic Sea, including Koper, extends from March
through May. It is noted for periods of stormy, winter-type
weather that alternate with false starts of settled
summer-type weather. Conditions moderate as the season
progresses.
- Some visibility restrictions
can occur with fog in the early spring. This is usually due
to a fog-laden west wind.
- Wind chill is a factor to be
considered for personnel working in exposed, outdoor
locations during early spring. When indicated, the Wind
Chill Table [see
https://www.nrlmry.navy.mil/~cannon/medports/Koper/windchilltable.html]
should be used to determine the equivalent wind chill
temperature for specific air temperature and wind speed
combinations.
Summer
- The summer season extends
from June through September. Summer weather in the northern
Adriatic Sea is generally warm and dry with light winds.
Strong Bora events are uncommon. The mild weather results
from the great continental low pressure area that replaces
the Eurasian winter anticyclone. The low is centered over
southwest Asia, with an extension westward over Asia Minor.
- Thunderstorms are most
frequent during the summer, but only average three or four
times per year. The storms occasionally form over the
coastal terrain and move over the port area. Thunderstorms
normally last only 2 to 4 hours in the Koper area.
Autumn
- The autumn season is short,
usually lasting about the month of October. The season is
characterized by an abrupt change to winter-type weather.
- Wind chill for personnel
working in exposed, outdoor locations is normally not a
factor until after October. When indicated, the Wind Chill
Table [see
https://www.nrlmry.navy.mil/~cannon/medports/Koper/windchilltable.html]
should be used to determine the equivalent wind chill
temperature for specific air temperature and wind speed
combinations.
- Thunderstorms are most
frequent during the summer, but may occur during autumn. The
storms occasionally form over the coastal terrain and move
over the port area. One strong November thunderstorm caused
northerly "Tramontana" winds of 108 kt (200 kph) at Koper.
Thunderstorms normally last only 2 to 4 hours in the Koper
area.
Winter
- Winter usually lasts for the
months of November through February. A great continental
anticyclone over Eurasia develops and extends southwestward
toward the Balkans. Cold Bora winds and clear weather (a
white Bora) usually result with this weather pattern as
transient extratropical low pressure systems over the
Mediterranean Sea cause strong pressure gradients to develop
over the Adriatic region on the south side of the
anticyclone. Stormy and unsettled weather at Koper may
accompany the Bora (a black Bora) when the low-pressure
systems move across the Adriatic Sea rather than farther
south over the Mediterranean Sea.
- Thunderstorms are most
frequent during the summer, but are possible all year. They
occasionally form over the coastal terrain and move over the
port area. A strong November thunderstorm caused a northerly
"Tramontana" wind gust of 108 kt (200 kph) at Koper.
Thunderstorms normally last only 2 to 4 hours in the Koper
area.
- Wind chill must be taken
into consideration when work is being performed in exposed,
outdoor locations during the winter season. The Wind Chill
Table [see
https://www.nrlmry.navy.mil/~cannon/medports/Koper/windchilltable.html]
should be used to determine the equivalent wind chill
temperature for specific air temperature and wind speed
combinations.
Protective or
Mitigating Measures
Moving to a New Anchorage
- Because Koprski Bay is
protected from most hazardous wave motion, wind will be the
dominating weather factor for ships anchored in Koprski Bay
or moored alongside berths in the Port of Koper. Waves
generated by Scirocco and Jugo winds do not reach the port
due to the protection afforded by the land mass south of
Koprski Bay. Bora winds blow seaward and do not have enough
fetch to generate bothersome wave heights in Koprski Bay.
During an intense Bora event, ships moored alongside a berth
should add lines to prevent excessive ship movement.
Anchored vessels, especially those that are empty, have
large sail areas, or do not have enough chain to provide an
adequate scope of anchor chain, should sortie from the port
because of the danger of anchor dragging. If remaining at
anchor, vessels should deploy an adequate scope of chain to
provide maximum holding strength on the mud bottom. Steaming
to the anchor during the strongest winds may be required.
- Positioning a vessel in the
lee of high terrain as close to the coastline as possible
will decrease the effect of the local seas during a severe
Bora. Territorial limits of the various countries bordering
the Adriatic Sea may prohibit taking maximum advantage of
this option, however. The evaluation of Trieste, Italy
recommends a location north of Castella Miramare, Italy,
moving to within one-half mile of the coast. This maneuver
will decrease seas substantially and decrease winds
slightly. Since there are mussel farms in this area,
up-to-date navigation charts must be consulted before
exercising this option.
Sortie/Remain in Port
- There is no sortie
information available for this port. The position of Koper
in the extreme northern part of the Adriatic Sea severely
limits sortie options.
Scheduling
- There is no scheduling
information available for this port.
Harbor Protection
- Wind and Weather:
- The Port of Koper is
vulnerable to frequent Bora wind events. During late
autumn, winter and early spring, in extreme events the
cold Bora winds can reach sustained velocities of 54 kt
(100 kph), with doubling of gust velocities. Some Bora
events last two to three days. Although Bora winds do
not normally cause problems for ships in port (most
berths are oriented east-west), additional mooring lines
may be required to keep a ship safely alongside her
berth. Bora winds are felt most strongly in Basin 3 and
in the entrance channel. The typical Bora wind direction
is approximately 060° in Basin 3 and in the channel, but
more easterly in Basins 1 and 2. Bora winds are most
commonly observed in the December through March period,
but they can occur during other months.
- Boras are classified
locally as being a "White Bora" or a "Black Bora." A
White Bora results when a strong pressure gradient
exists between a cold high pressure area north of
Slovenia and a low pressure area over the Mediterranean
Sea. A White Bora is characterized by cold, clear
weather and very gusty winds. A Black Bora results when
the low pressure area is located over the Adriatic Sea
so that the weather over Slovenia is cloudy and rainy.
Black Bora winds are less gusty than those in a White
Bora.
- Anchor dragging is
possible during a strong Bora event. Those vessels
opting to remain at anchor at Koper should deploy enough
scope of chain to provide maximum holding strength on
the mud bottom. Steaming to the anchor may be required
to prevent anchor dragging during the strongest winds.
Positioning a vessel in the lee of high terrain as close
to the coastline as possible will decrease the effect of
the local seas during a Bora event.
- Koper is also affected by
other wind events, including Scirocco, Jugo and
Maistral. Scirocco directions vary from southeast to
south-southwest. Because of their direction being
more-or-less perpendicular to the channel orientation,
they can cause handling problems for ships in the
channel. When Scirocco conditions prevail, a location
just northeast of Petelinji Point is recommended as an
anchorage at Koper. Jugo winds are southwesterlies, and
also cause handling problems for ships in the channel.
An anchorage in Koprski Bay approximately midway between
Debeli Point and Petelinji Point is the recommended
anchorage when Jugo winds occur. The Maistral is a
northwesterly wind that occurs during the warm months of
late spring, summer and early autumn. Maistral speeds
are usually in the 11-16 kt range, so they pose little
problem to vessels at the Port of Koper.
- Thunderstorms are possible
at Koper year-round, but are most frequent during
summer. Such storms can be intense, with one strong
November storm causing a northerly "Tramontana" wind
gust of 108 kt (200 kph) at Koper.
- Waves:
- Due to limited fetch, Bora
winds do not raise problem waves at the Port of Koper. A
sustained southerly or south-southwesterly Scirocco
event can raise seas of 6.6 to 9.8 ft (2 to 3 m) in the
open water west of Koper, but waves in Koprski Bay are
fetch limited by the land mass south of the bay. When
such conditions occur, departing vessels up to 1,500 GWT
often anchor in Piranski Bay to wait until the winds and
waves over the Adriatic Sea abate. Piranski Bay is
located approximately 8 nmi west-southwest of the Port
of Koper.
Local Hazardous Weather
Conditions
- Wind and Weather: Koper's
climate is dominated by the Bora wind, which can occur
anytime during the year. However, the peak frequency occurs
in the cold season (November - March). To a lesser extent,
the Scirocco wind affects Koper but is not nearly as strong
or as frequent as the Bora. Gulf of Genoa lows have an
influence on weather in the northern Adriatic Sea as they
either move toward Koper causing stormy weather with clouds
and rain, or they move southeastward causing a steep
pressure gradiant over at Koper, initiating a Bora outbreak.
Bora: Bora winds result when
cold air accumulates over the Balkan Peninsula,
especially the region between Albania and Austria. When
the depth of the cold air pool reaches the height of
mountain passes, the Bora will commence.
- There are two primary
weather patterns associated with the Bora:
- Anticyclonic pattern: A
large high pressure cell is present over central Europe
without a well defined low pressure center to the south.
- Cyclonic pattern: A low
pressure center is present in the southern Adriatic Sea
or in the Ionian Sea. In either case, the pressure is
higher on the European side of the mountains and lower
on the Mediterranean side.
- The Bora is most common in
the Adriatic Sea where it flows mainly from the northeast
through gaps in the Dinaric Alps. One of these gaps is near
Trieste and is known as the Trieste Gap. The gap east of
Koper is not as prominent as the Trieste Gap. On occasion,
the Bora can be very localized, extending only a few miles
offshore. At other times, the Bora will dominate the entire
Adriatic Sea and, when the area of steep pressure gradiant
is large enough, the Bora can extend as far south as Malta.
- In the northern Adriatic
Sea, the wind direction associated with the Bora is
generally northeasterly but can vary in local areas due to
the terrain. The Bora at Koper and Trieste is
east-northeasterly. It is more northerly farther south and
even northwesterly along Italy's southeast coast.
The strongest winds occur
along the eastern shore of the Adriatic Sea from Trieste
to the Albanian border.
Anticyclonic pattern Bora
winds are most intense to the north, decreasing somewhat
moving southward.
The greatest intensity of
the Bora occurs where the mountain peaks are at least
2000 ft above sea level and not more than two or three
miles inland.
Winds are usually less
intense over the open water of the Adriatic Sea, but
gale force winds (greater than or equal to 34 kt) are
common. The frequency of the gale force Bora in the open
sea is greater for the cyclonic type of pattern than for
the anticyclonic pattern.
During the cyclonic
pattern, the strongest winds are usually found in the
southern Adriatic Sea.
Bora winds are most common
during the cool season (November through March). In
general, the frequency of gale force winds varies from
one day per month, or less, in the summer to six days
per month during winter months.
The average duration of a
continuous gale force Bora over the Adriatic Sea is
about 12 hours but the winds sometimes will last up to
two days.
The average duration of a
Bora that reaches gale force some time during its
history is 40 hours with a maximum duration of 5 days.
At Koper, the average
duration of a gale force Bora varies from three days in
winter to one day in summer. Local mariners state that
the Bora will last an odd number of days; 1, 3, 5, etc.
However, the Bora has been known to last for up to 30
days at Trieste without a significant lull.
In 1956 a gust of 125 kt
was recorded at Trieste.
The Bora does not usually
start with a sudden blast but will build up at a
relatively moderate pace. A 60 kt Bora will not reach
peak intensity during the first 3 or 4 hours. This may
allow time for some protective measures to be assessed
and conducted.
Wave heights near the port
of Koper are normally not high with a Bora because they
are fetch limited.
There is a noticeable
diurnal variation at stations along the eastern coast of
the Adriatic Sea during Bora conditions. During the day,
the sea breeze counteracts the offshore flow of the
Bora, which decreases the strength of the Bora between
1200L and 1800L.
With the anticyclonic
pattern, the Bora is basically a dry wind due to its
katabatic nature. Clear skies and good visibilities are
found in the lee of the mountains while thick clouds
associated with up-slope motions are found on the
mountain crests. These clouds subsequently dissipate in
the descending air on the lee side, and appear as "cap
clouds" to an observer on their west side.
With the cyclonic pattern,
the Bora is often accompanied by low clouds and reduced
visibilities associated with rain and/or drizzle. These
conditions are more noticeable over the open water areas
than along the coastal zone.
- Scirocco: The Scirocco is a
southeasterly to south-southwesterly wind over the
Mediterranean originating over North Africa, sometimes
affecting the Adriatic Sea area.
The Scirocco tends to occur
year-round without a favored month or season.
The Scirocco normally
occurs within the warm sector of a cyclone passing
either north or west of the region. These cyclones
originate either over North Africa or south of the Alps,
primarily in the Gulf of Genoa in the latter case.
Scirocco conditions occur
in the Gulf of Genoa case when the circulation extends
far enough southward to draw air from the North African
region.
The onset of the Scirocco
is more gradual than the onset of a Bora. It occurs more
frequently in the southern part of the Adriatic Sea with
a decrease in frequency northward.
Although the Scirocco is
not as strong as the Bora, winds can reach gale force
(greater than or equal to 34 kt), especially in winter
and spring.
The average duration of
continuous gale force winds during a Scirocco is 10 to
12 hours and occasionally as long as 36 hours. The
maximum wind speed likely during a Scirocco is about 55
kt. Local terrain features alter the effect of the
Scirocco. Winds will parallel the coast in general.
As a cold front approaches
from a relatively flat, low surface, such as the ocean,
toward an elevated land mass, super-gradient winds will
occur due to the Venturi effect. These winds are
restricted to a narrow band between the front and the
landmass and do not normally sustain for long periods of
time. Seas are usually not high with strong
southeasterlies due to protection from the terrain, but
sustained Scirocco winds can raise seas of 6.6 to 9.8 ft
(2 to 3 m) in the open water west of Koper. Waves in the
harbor are fetch limited.
- Genoa Lows: Genoa lows are
low-pressure systems which develop to the south of the Alps
in the region incorporating the Gulf of Genoa, Ligurian Sea,
Po Valley, Gulf of Venice and northern Adriatic Sea.
Although several factors are important in cyclogenesis, the
development of the cyclone near the Gulf of Venice--as
opposed to the west near the Gulf of Genoa--depends on the
amount of cold air penetrating the Po Valley from the
northeast. If there is little or no cold air entering the Po
Valley, the low will probably form in the Gulf of Venice;
otherwise, cyclogenesis will occur to the west. Genoa
cyclones usually remain stationary (or at least leave a
residual trough) south of the Alps throughout their life
history. If the lows do move, they generally follow one of
two tracks.
The first track, common for
cyclones developing in the Gulf of Venice, is a
northeasterly to north-northeasterly direction across
the Alps. This track is associated with strong
southwesterly flow aloft. In this case, Scirocco
conditions are likely if the circulation of the low
extends southward into North Africa, allowing air from
the desert source to move northward.
The second track,
associated with a strong anticyclone over the Balkans,
Turkey and the Black Sea, is in a southeasterly
direction from the Gulf of Genoa towards the Ionian Sea.
In this case, a gale force Bora is extremely likely by
the time the depression moves into the Ionian Sea.
Heat Index and Windchill
Charts
Source:
|
Main
Menu
Created: Wednesday, April
18, 2007; Updated:
Saturday, January 01, 2022
Copyright © 1998
IstriaNet.org, USA
|
|