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False Bay

Bay of the Atlantic Ocean at South Africa

  • 57 min read
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Through Island, Tide and El Niño–Southern Oscillation

False Bay is at the extreme western end of the inshore Agulhas marine ecoregion, which extends from Cape Point to the Mbashe river over the continental shelf, in the overlap zone between Cape Agulhas and Cape Point, where the warm Agulhas Current and the cooler South Atlantic waters mix. The continental shelf is at its widest in this ecoregion, extending up to 240 km (150 mi) offshore on the Agulhas Bank, but is considerably narrower off False Bay. This ecoregion has the highest number of South African marine endemics and is a breeding area for many species. The transition between the Agulhas ecoregion and the cooler Benguela ecoregion is at Cape Point, on the western boundary of False Bay.

False Bay also contains South Africa's largest naval base at Simon's Town (historically a base for the Royal Navy), and small fishing harbours at Kalk Bay and Gordon's Bay.

Description and location

The western side is bordered by the Cape Peninsula, and this stretch of coastline includes the smaller Buffels Bay, Smitswinkel Bay, Simon's Bay, and Fish Hoek Bay. At Muizenberg, the coastline becomes relatively low and sandy and curves east across the southern boundary of the Cape Flats to Gordon's Bay, to form the northern boundary of False Bay. From Gordon's Bay, the coastline swings roughly south and zigzags along the foot of the Hottentots Holland Mountains to Cape Hangklip, which is at nearly the same latitude as Cape Point. The highest peak on this side is Kogelberg at 1,269 m (4,163 ft).

The bay is approximately square-shaped with wobbly edges, with roughly the same length from north to south as from east to west (30 km (19 mi)), with the entire southern side open to the ocean. The area of False Bay has been measured at about 1,090 km2 (420 sq mi), and the volume is approximately 45 km3 (11 cu mi) (with an average depth of about 40 m (130 ft)). The land perimeter has been measured from a 1:50,000-scale map at 116 km (72 mi).

The eastern and western shores of the bay are very rocky and even mountainous; in places, large cliffs plunge into the water. Notable peaks associated with the bay include Koeëlberg (1,289 m (4,229 ft)), which rises from the water itself and forms the highest point of the Kogelberg, as well as Somerset Sneeukop (1,590 m (5,220 ft)) and Wemmershoek Peak (1,788 m (5,866 ft)), which are clearly visible across the bay. Some of the highest peaks visible across False Bay include Du Toits Peak near Paarl (1,995 m (6,545 ft)), Klein Winterhoek Peak near Tulbagh (1,995 m (6,545 ft)), Mostertshoek Peak at the Western extreme of the Michell's Pass (2,008 m (6,588 ft)) and Groot Winterhoek Peak North of Tulbagh (2,077 m (6,814 ft)). The northern shore is defined by a very long, curving, sandy beach. This sandy northern perimeter of the bay marks the southern edge of the Cape Flats. The bay is 30 km (19 mi) wide at its widest point.

Suburbs of Cape Town stretch right across the Cape Flats, from Simon's Town halfway down the Cape Peninsula to the north-eastern corner at Gordon's Bay. There are also two small towns of the Overberg region on the east coast of the bay, Rooiels and Pringle Bay.

Coastal landmarks

The coastal landmarks visible from offshore in False Bay, listed clockwise from Cape Point to Cape Hangklip, are:

  • Cape Point, 34°21′26″S 18°29′51″E / 34.35722°S 18.49750°E, the south-westernmost point of the bay, marked by the current lighthouse and the original lighthouse,
  • Vasco da Gama Peak (266m), 34°20′41.07″S 18°28′29.32″E / 34.3447417°S 18.4748111°E, the highest point nearest the mouth of the bay on the Cape Peninsula,
  • Rooikrans, 34°20.456′S 18°28.407′E / 34.340933°S 18.473450°E, A cliff area with a small sea cave,
  • Matrooskop (109m), 34°19.576′S 18°27.834′E / 34.326267°S 18.463900°E, a small local peak inshore of Buffels Bay,
  • Buffels Bay, 34°19.123′S 18°27.650′E / 34.318717°S 18.460833°E, a small bay on the west side of False Bay, with a small craft slipway,
  • Bordjiesrif, 34°18.876′S 18°27.782′E / 34.314600°S 18.463033°E, a small, low sandstone promontory on the north side of Buffels Bay,
  • Paulsberg (369m), 34°17.635′S 18°27.808′E / 34.293917°S 18.463467°E
  • Judas Peak (319m), 34°16.7′S 18°28.3′E / 34.2783°S 18.4717°E, the peak above the cliffs to the immediate south of Smitswinkel Bay,
  • Batsata Rock, 34°16.603′S 18°28.836′E / 34.276717°S 18.480600°E, an exposed inshore granite rock below Judas Peak near the northern boundary of the Paulsberg restricted zone, and the southern limit of Smitswinkel Bay,
  • Smitswinkel Bay, 34°16.007′S 18°28.261′E / 34.266783°S 18.471017°E, a small bay on the west side of False Bay, with a few coastal houses,
  • Baboon Rock, 34°15.466′S 18°28.339′E / 34.257767°S 18.472317°E, a landmark indicating the southern extent of the Castle Rock restricted area,
  • Partridge Point, 34°15.343′S 18°28.606′E / 34.255717°S 18.476767°E, a granite corestone promontory with several large exposed inshore rocks extending about a hundred metres into the bay on the north side of Smitswinkel Bay,
  • Finlay's Point, 34°14′56.9″S 18°28′36.5″E / 34.249139°S 18.476806°E, a smaller granite corestone promontory north of Partridge Point,
  • Castle Rocks, 34°14.362′S 18°28.661′E / 34.239367°S 18.477683°E, a larger granite corestone promontory, comprising a massive and fairly high outcrop at the end of a small, low isthmus, with several large inshore exposed rocks south of Miller's Point,
  • Bakoven Rock, 34°14.040′S 18°29.012′E / 34.234000°S 18.483533°E, an exposed inshore granite rock between Castle Rocks and Miller's Point, near the northern extent of the Castle Rocks restricted area,
  • Rumbly Bay, 34°14.020′S 18°28.489′E / 34.233667°S 18.474817°E, a small cove with a small craft slipway on the south side of Miller's Point,
  • Miller's Point, 34°13.932′S 18°28.587′E / 34.232200°S 18.476450°E, a fairly large but low granite corestone promontory, with a small craft slipway on the northwest side, and several exposed and drying rocks extending to seaward,
  • Spaniard Rock, 34°13.030′S 18°28.017′E / 34.217167°S 18.466950°E, an inshore exposed granite rock off Rocklands Point,
  • Rocklands Point, 34°12.964′S 18°27.921′E / 34.216067°S 18.465350°E, a minor granite promontory north of Miller's Point,
  • Swartkop (679m), 34°12.943′S 18°27.025′E / 34.215717°S 18.450417°E, the highest point on the Southern Peninsula,
  • Simonsberg (548m), 34°12.299′S 18°26.304′E / 34.204983°S 18.438400°E, the peak above Simon's Town,
  • Oatlands Point, 34°12.067′S 18°27.395′E / 34.201117°S 18.456583°E, a minor granite promontory with a large inshore exposed rock and a shoreline navigation beacon,
  • Fishermans Beach, , a short, sandy beach north of Oatlands Point,
  • Froggy Pond, 34°12.219′S 18°27.418′E / 34.203650°S 18.456967°E, a small cove with a small sandy beach north of Fishermans Beach separated by a low rocky promontory,
  • Windmill Beach, 34°12.067′S 18°27.395′E / 34.201117°S 18.456583°E, a small sandy beach partly enclosed by massive granite boulders, with two small coves,
  • Noah's Ark rock, 34°11.533′S 18°27.231′E / 34.192217°S 18.453850°E, a conspicuous inshore exposed rock at the mouth of Simon's Bay,
  • Simon's Bay, 34°11.073′S 18°25.945′E / 34.184550°S 18.432417°E, the largest bay on the west side of False Bay, very well protected from the prevailing south westerly swell, but fairly exposed to wind and waves from the south-east,
  • Boulders Beach, Seaforth, 34°11.833′S 18°27.082′E / 34.197217°S 18.451367°E, a sandy beach between large scattered granite boulders,
  • Simon's Town Naval Base harbour, 34°11.317′S 18°26.283′E / 34.188617°S 18.438050°E, an artificial harbour with breakwater and sea-walls enclosing the naval dockyard,
  • False Bay Yacht Club moorings, 34°11.427′S 18°26.015′E / 34.190450°S 18.433583°E, a floating marina protected from the south-easterly wind and waves by the naval harbour, with somewhat less protected open moorings further into the bay,
  • Long Beach, 34°11.236′S 18°25.579′E / 34.187267°S 18.426317°E, a sandy beach on the west side of Simon's Bay, usually in the lee of the harbour for south easterly winds,
  • Roman Rock, 34°10.877′S 18°27.606′E / 34.181283°S 18.460100°E, an exposed rock in Simon's Bay with a lighthouse on it,
  • Mackerel Bay, 34°10.302′S 18°25.761′E / 34.171700°S 18.429350°E, a small sandy beach north of Simon's Town,
  • Glencairn, 34°9′48″S 18°25′47″E / 34.16333°S 18.42972°E, a small residential suburb in a valley north of Simon's Town, with a beach in Elsebaai,
  • Elsebaai, 34°09.593′S 18°25.921′E / 34.159883°S 18.432017°E, a small bay in the north part of Simon's Bay,
  • Glencairn quarry, 34°09′13″S 18°26′11″E / 34.15366°S 18.43629°E, a conspicuous excavation in the side of Else Peak,
  • Else Peak (303m), 34°09.000′S 18°26.113′E / 34.150000°S 18.435217°E, a small peak between Simon's Town and Fish Hoek,
  • Fish Hoek bay, 34°08′15″S 18°26′01″E / 34.13745°S 18.43374°E, the northernmost minor bay of the west side of False Bay with a sandy beach open to the sea,
  • Sunny Cove, 34°08.661′S 18°26.239′E / 34.144350°S 18.437317°E, the rocky sandstone coastline on the south side of Fish Hoek bay,
  • Fish Hoek beach, 34°08.160′S 18°26.148′E / 34.136000°S 18.435800°E, a sandy beach on the east side of the Fish Hoek–Noordhoek gap, a low-lying break in the mountain range of the peninsula between False Bay and the Atlantic coast.
  • Trappieskop, 34°07.668′S 18°26.414′E / 34.127800°S 18.440233°E, the hill above Kalk Bay,
  • Kalk Bay harbour, 34°07.698′S 18°26.986′E / 34.128300°S 18.449767°E, a small commercial fishing harbour in Kalk Bay, completely enclosing the tiny sandy beach,
  • St James, 34°7′8″S 18°27′33″E / 34.11889°S 18.45917°E, the suburb to the north of Kalk Bay,
  • Kalkbaaiberg (517m), 34°06.737′S 18°26.382′E / 34.112283°S 18.439700°E, the peak above Kalk Bay,
  • Muizenberg (509m), 34°06.006′S 18°27.556′E / 34.100100°S 18.459267°E, the peak to the west of Muizenberg suburb, and the northernmost peak directly overlooking the west side of False Bay,
  • Muizenberg beach (Sunrise Beach), 34°06′04″S 18°29′22″E / 34.10120°S 18.48948°E, a long sandy beach along the low-lying northwestern coast of False Bay,
  • Kapteinsklip, 34°04.726′S 18°37.249′E / 34.078767°S 18.620817°E, a low rocky promontory between Muizenberg and Strandfontein beaches,
  • Strandfontein, 34°05.326′S 18°33.204′E / 34.088767°S 18.553400°E,
  • Wolfgat Nature Reserve, 34°04′11″S 18°38′54″E / 34.0697°S 18.6482°E, a small coastal nature reserve on the north coast of the bay,
  • Swartklip, 34°04.477′S 18°41.118′E / 34.074617°S 18.685300°E,
  • Monwabisi, 34°04′22″S 18°41′10″E / 34.072853°S 18.686209°E, a resort area on the north coast of the bay,
  • Macassar Beach, 34°04′35″S 18°45′08″E / 34.07643°S 18.75224°E, a long stretch of sand beach on the north coast of the bay,
  • Eerste River mouth, 34°04.873′S 18°45.887′E / 34.081217°S 18.764783°E, the mouth of the largest river crossing the Cape Flats,
  • Helderberg Marine Protected Area, 34°05′S 18°47′E / 34.083°S 18.783°E, a small coastal marine protected area between the mouths of the Eerste and Lourens rivers,
  • Lourens River mouth, 34°06.005′S 18°48.706′E / 34.100083°S 18.811767°E, the mouth of the river flowing through Somerset West and Strand,
  • Strand Beach, 34°06′20″S 18°49′04″E / 34.10554°S 18.81776°E, a sandy shoreline along the coast of the suburb, becoming rocky to the east,
  • Harbour Island marina, 34°09.097′S 18°51.356′E / 34.151617°S 18.855933°E, a small craft harbour development on the north-eastern coast of the bay,
  • Gordon's Bay beach, 34°09.499′S 18°52.070′E / 34.158317°S 18.867833°E, a small sandy beach in the north-eastern corner of the bay,
  • Gordon's Bay Harbour, 34°09.801′S 18°51.504′E / 34.163350°S 18.858400°E, a small fishing harbour and marina,
  • Steenbras River mouth, 34°11.671′S 18°49.194′E / 34.194517°S 18.819900°E, mouth of a river with catchment to the east of the Hottentots Holland range,
  • Boskloof Peak (648m), 34°12′15.12″S 18°50′20.04″E / 34.2042000°S 18.8389000°E, mountain peak south of the Steenbras River mouth,
  • Boskloof Point, 34°13.028′S 18°49.777′E / 34.217133°S 18.829617°E, promontory south of the Steenbras River mouth,
  • Kogelbaai, 34°14′02″S 18°50′56″E / 34.23397°S 18.84900°E, a fairly long sandy beach on the east coast of the bay,
  • Kogelberg, 34°13.880′S 18°53.253′E / 34.231333°S 18.887550°E, a mountain peak above Kogelbaai,
  • Rooielsberg (638m), 34°16.960′S 18°50.112′E / 34.282667°S 18.835200°E, a peak above the point to the north of Rooi-Els,
  • Rooi-Els River mouth, 34°17.848′S 18°49.20′E / 34.297467°S 18.82000°E, the mouth of the Rooi-Els river at a small sandy beach in Rooi-Els bay,
  • The Point (Rooi-Els), 34°17′51″S 18°48′50″E / 34.29750°S 18.81389°E,
  • Klein Hangklip (309m), 34°18′26″S 18°49′19″E / 34.30722°S 18.82194°E, a small peak overlooking Rooi-Els,
  • Rooi-Els, 34°18′05″S 18°48′59″E / 34.30139°S 18.81639°E, a small coastal residential area in the Overberg district,
  • Pringle Bay, 34°20′31″S 18°49′16″E / 34.34194°S 18.82111°E, A small, shallow bay on the south-east side of False Bay, which has a small sandy beach on the east and a rocky coastline to the south, with a small residential town along the shore,
  • Buffels River mouth, 34°20′20″S 18°40′47″E / 34.33889°S 18.67972°E, the mouth of a small river, draining into Pringle Bay,
  • Die Punt (Pringle Bay), 34°20′55″S 18°48′38″E / 34.34861°S 18.81056°E, The point to the south of Pringle Bay,
  • Pringle Peak (159m), 34°21′4.17″S 18°49′18.37″E / 34.3511583°S 18.8217694°E, Peak at Pringle Bay,
  • Hangklip (455m), 34°21.919′S 18°49.700′E / 34.365317°S 18.828333°E, peak at the south eastern extreme of False Bay, with near vertical profile on the south side,
  • Cape Hangklip, 34°21′13″S 18°49′39″E / 34.35361°S 18.82750°E, a low promontory extending southwards below Hangklip Peak,

Bottom morphology

The bottom morphology of False Bay is generally smooth and fairly shallow, sloping gently downwards at about 3 m per km from north to south, so that the depth at the centre of the mouth is about 80 m (260 ft). The bottom is covered with sediment, ranging from very coarse to very fine, with most of the fine sediment and mud in the center of the bay. The main exception is a long ridge of sedimentary rock that extends southward from off the Strand to approximately level with the mouth of the Steenbras River. The southern tip of this ridge is known as Steenbras Deep.

There is one true island in the bay, Seal Island, a barren and stony outcrop of granite about 200 m (660 ft) long and with an area of about 2 ha (24,000 sq yd). It is about 6 km (3.7 mi) south of Strandfontein and is less than 10 m (33 ft) above sea level at its highest point. Many small rocky islets extend above the high-water mark, and other rocks and shoals that approach the surface. The largest of these, and the most significant navigational hazard in the bay, is Whittle Rock, a large outcrop of granite about halfway into the bay and a quarter of the way across from the Cape Peninsula (34°14.846′S 18°33.714′E / 34.247433°S 18.561900°E), which is about 1 km (0.62 mi) in diameter and rises from a fairly flat sand bottom at about 40 m (130 ft) to within 4 m (13 ft) of the surface. There are smaller outlying granite reefs scattered to the south, east, and west of Whittle Rock, and more smaller granite reefs to the northwest. Most of the reefs on the western side of the bay are composed of granite from the Peninsula pluton. Still, east of Seal Island, they are generally sandstone, either of the Table Mountain series, or of the underlying Tygerberg formation. Whittle Rock reef can refract large south easterly storm waves, increasing their size in the vicinity of Kalk Bay harbour.

Other shoal areas include the granite reefs at Roman Rock in Simon's Bay, hard sedimentary or metamorphic rock at York shoal and hard sandstone at East shoal, and several isolated granite outcrops which are too deep to be navigational hazards in the western part of the bay. The palaeo-drainage of the bay is split between the western side of the bay and the eastern side by the relatively durable contact zone between the Peninsula granite and the Tygerberg sediments, with deep valleys cut into the bedrock during the glacial maximum, which have since been filled with sediments. The drainage of the west side passed to the west of Seal Island, Whittle Rock, and Rocky Bank. The east side was drained by a valley between Seal Island and East Shoal, and another valley to the east of Steenbras Ridge, which joined east of Rocky bank and exited the bay between Rocky Bank and Hangklip Ridge.

Outside the bay, but influencing the wave patterns in it, Rocky Bank is an extensive area of relatively flat sandstone reef between 20 and 30 m (66 and 98 ft) deep on the top, sloping down on all sides, but mostly to the south and east, where the depth can exceed 100 m (330 ft). A long underwater sandstone ridge sweeps across the eastern side of the mouth from Cape Hangklip towards the southwest, which is believed to affect water circulation in the bay. On the west side, a relatively shallow area of granite reef extends beyond the Cape Peninsula, with one major navigational hazard at Bellows Rock and a lesser one somewhat closer inshore at Anvil Rock.

Bathymetry

The bathymetry of False Bay differs from that of the west side of the Cape Peninsula. The west coast seabed tends to slope down more steeply than in False Bay and, although the close inshore waters are also shallow, the 100 m (330 ft) contour is mostly within about 10 km (6.2 mi) of the west coast, while the entire False Bay is shallower than about 90 m (300 ft). The bottom of the bay slopes down relatively gradually from the gently sloping beaches of the north shore to the mouth, and has a fairly even depth from east to west except close to the shorelines, with three major features disrupting this gentle slope. These are Seal Island, Whittle Rock, and the Steenbras ridge. Just outside the bay, there is a large shoal area at Rocky Bank, and a large ridge extending south-west from Cape Hangklip, which channels cold, nutrient-rich water into the west side of the bay during upwelling events.

Geology

The three main rock formations are the late-Precambrian Malmesbury Group (sedimentary and metamorphic rock), the Peninsula granite, a huge batholith that was intruded into the Malmesbury Group about 630 million years ago, and the Table Mountain group sandstones that were deposited on the eroded peneplain surface of the granite and Malmesbury series basement about 450 million years ago. The sand, silt, and mud deposits were lithified by pressure and then folded during the Permian–Triassic Cape Orogeny to form the Cape Fold Belt, which extends along the western and southern coasts of the Western Cape. The present landscape is due to prolonged erosion, which has carved deep valleys, removed parts of the once-continuous Table Mountain Group sandstone cover from the Cape Flats, and left high residual mountain ridges.

At times, the sea covered the Cape Flats and Noordhoek valley, the Cape Peninsula was then a group of islands, and False Bay and the Cape Flats a strait. During glacial periods, the sea level dropped, exposing the bottom of False Bay to weathering and erosion; the last major regression left the entire bottom of False Bay exposed. During this period, an extensive system of dunes was formed on the sandy floor of False Bay. At this time, the drainage outlets lay between Rocky Bank and Cape Point to the west, and between Rocky Bank and Hangklip Ridge to the east.

Waves, tides, water circulation, and temperature

Swell entering the bay is predominantly the product of the westerly winds blowing over the Southern Ocean. The prevailing swell is about 12 to 25 seconds in period from the southwest, with an average height of about 3 m (9.8 ft). It impinges directly on the east coast of the bay, amplified by refraction over Rocky Bank in the region near the Steenbras River mouth, where rogue waves may occur. Further west, the swell refracts and diffuses around a fairly large shoal area around Cape Point, and is moderately to severely attenuated by the time it reaches the western shores.

Waves along the north coast of the bay between Macassar and Muizenberg generally break by spilling as the slope is gradual. In summer, strong south-easterly winds blow over a fetch partly limited by the width of the bay and generate short-period wind waves of around 6 seconds and 2 m (6.6 ft) height, and produce multiple lines of breakers along the north shore. Where the slopes are steeper, rip currents may form, posing a hazard to swimmers.

Northward propagating long period waves are focused in the northeast and northwest parts of False Bay by refraction effects over the shoal waters of Rocky Bank in the mouth of the bay, with measured heights of waves in the area between Steenbras mouth and Kogelbaai being up to twice the height of the waves in the Muizenberg to Strandfontein region for the prevailing southwesterly open ocean swell. The focusing effect is mostly on swells with a period of 13 seconds or more, and a direction between 210° and 245° true. The smaller and shallower reef at Whittle Rock towards the west side of the bay has a similar but lesser effect, and can focus longer period south-easterly waves on Kalk Bay. This is unusual, and associated with a cut-off low-pressure system causing the south-easterly winds to blow for an unusually long time over enough fetch to develop a sea sufficiently for it to be refracted by the shoal area. Wave height of southwesterly swells decreases from west to east along the north coast of False Bay from around Macassar to Gordon's Bay due to the effects of refraction and friction of the wave base on larger areas of offshore reef before reaching the shoreline.

Tides are regular, semi-diurnal, and relatively weak, and there are no strong tidal currents. Maximum tidal range at Simon's Town is 2 m (6.6 ft) at the highest astronomical tide, with a minimum range of about 0.56 m (1.8 ft) at mean neap tides. When large waves break at Macassar on a high tide, the beach is known to be dangerous for swimming, and beach erosion is increased.

The circulation patterns in False Bay are variable over time, with seasonal and longer-term cycles. There are cold-water upwelling events associated with south-easterly winds in summer, and periodic intrusions of warm-water eddies from the Agulhas Current along the south coast, both of which contribute to biodiversity.

Four main surface circulation patterns have been observed in False Bay. Wind is the dominant forcing influence on surface circulation, with tidal and inertial currents of secondary importance, mainly when the winds are weak. Gordon's Bay is in the wind shadow of the Hottentots-Holland Mountains for south easterly winds, and this causes a semi-permanent anticyclonic eddy and associated anticlockwise gyre, in the opposite direction to the usual cyclonic circulation of the main part of the bay.

A clockwise rotation driven by the south-easterly winds mostly occurs during summer. This circulation is partly set up by the west-northwesterly flow south of the bay, which splits at Cape Point. The northerly component sets up flow towards the equator on the western shores. South-easterly winds cause this clockwise pattern to dominate. North-westerly winds cause an anti-clockwise circulation, with an eastward current flowing south of the Bay and entering at Cape Hangklip. When there is no strong wind forcing, tidal forcing can occur on the incoming and outgoing tides. A fairly uniform northward flow occurs during flooding tides, and southward during ebbing tides, with bathymetry affecting the flow direction in shallow areas. These currents are most noticeable along the coastline and in the shallow northern parts of the bay between Simon's Town and Gordon's Bay.

In the deeper areas of the mouth of the bay, tidal and inertial currents appear to contribute to the variability of the deeper part of the water column, along with the effects of wind forcing. Wave energy focused by the various shoal areas outside and inside the bay is a driver of nearshore currents, particularly in the northern parts of the bay.

In summer, False Bay is thermally stratified, with a vertical temperature range of 5 to 9 °C (41 to 48 °F) between the warmer surface waters and the cooler waters below 50 m (160 ft). In contrast, in winter, the water column is nearly constant in temperature at all depths. The development of a thermocline is strongest around late December and peaks in late summer to early autumn. In summer, the south easterly winds generate a zone of upwelling near Cape Hangklip, where surface water temperatures can be 6 to 7 °C (43 to 45 °F) colder than the surrounding areas, and bottom temperatures below 12 °C (54 °F).

In the summer to early autumn (January–March), cold water upwelling near Cape Hangklip causes a strong surface temperature gradient between the south-western and north-eastern corners of the bay. In winter, the surface temperature tends to be much the same everywhere. In the northern sector, surface temperatures vary a bit more (13 to 22 °C (55 to 72 °F)) than in the south (14 to 20 °C (57 to 68 °F)) throughout the year.

Surface temperature variation from year to year is linked to the El Niño–Southern Oscillation. During El Niño years, the South Atlantic high is shifted, reducing the south-easterly winds, so upwelling and evaporative cooling are reduced, and sea surface temperatures throughout the bay are warmer, while in La Niña years, there is more wind and upwelling and consequently lower temperatures. Surface water heating during El Niño increases vertical stratification. The relationship is not linear.

Water density dynamics are mostly temperature dependent, with only weak influences from salinity. The major influence on the temperature distribution is wind-driven upwelling and advection of cold water, which is most notable north-west of Hangklip and less marked near Gordon's Bay, due to strong south-easterly winds, with isolation as a secondary effect, mostly in the shallow waters of the northern and north-easterly regions. Waves may have a greater influence on nearshore temperatures than wind. Upwelling outside the bay along the coast east of Hangklip can also supply cold water to the bay.

Rivers and drainage

Drainage into False Bay can be considered from four watersheds: the east-flowing streams of the southern Cape Peninsula, the Cape Flats, the Helderberg basin, and the south-westwards drainage of the Hottentots-Holland mountains of the Overberg, extending south as far as Cape Hangklip.

The eastward draining rivers of the Southern Peninsula are generally fairly short and steep, and some, such as the Silvermine and Elsje rivers, have valley bottom wetlands at the coast. The Buffels River flows from a small spring to its mouth in Buffels Bay; the Klawersvlei River flows northwest from behind the mountains above Miller's Point over the plateau behind Simon's Town, before turning east over the escarpment and a high waterfall, entering the bay near the Simon's Town railway station; the Elsjes River flows from the Red Hill plateau to enter False Bay from the Glencairn valley; and the Silvermine River, originally known as the Esselstein River, drains the valley south of the Steenberg mountains and flows east across the Steenberg Plateau, then south through the Silvermine Valley before crossing the coastal Fish Hoek plain to enter False Bay at Clovelly on the north side of Fish Hoek Bay. Between these short and fairly steep streams, rainwater runoff generally flows directly down the mountainside into the bay.

The Sandvlei catchment drains the east side of the mountains north of Muizenberg and south of the Liesbeek catchment into False Bay: Sandvlei (Zandvlei) is the largest of eight estuaries on the False Bay coastline, with an area of about 155 ha (0.60 sq mi). The Westlake, Keysers, and Sand rivers feed it. The southern Diep River flows from the mountains above Constantia to Little Princessvlei, which drains into the Sand River, which flows into the northeast of Sandvlei. The Westlake River, also known as the Steenberg or Raapkraal River, originates on the slopes of the Steenberg and flows through the Kirstenhof wetlands into the north-west of Sandvlei. The Keysers River and its tributaries, the Grootbosch, Spaanschemat, and Prinseskasteel rivers, rise on Constantiaberg. The upper reaches of the Spaanschemat River are known as the Glen Alpine Stream, which originates below Constantia Nek and is joined by the Eagles Nest Stream.

Historically, the Cape Flats was partly covered in wetlands, particularly during winter, and retained much of its rainfall. Many of these wetlands have been destroyed by canalization and infilling to provide residential space. Many of the remaining perennial vleis are at the southwest side of the region (Zeekoevlei, Rondevlei, Zandvlei, etc.) and drain into the bay at Muizenberg through the estuary at Zandvlei. There is also groundwater seepage through the sand along the bay's north coast. The Elsieskraal River and the Black River catchment drain to the northwest into Table Bay, and do not affect False Bay. The Diep River catchment drains into Zandvlei, and Zeekoevlei and its catchment also drain to Zandvlei at times.

The Eerste River and its tributary, the Kuils River, drain into False Bay on the north coast, west of the Helderberg basin watershed. They drain part of the Cape Flats, but most of the catchment of the Eerste River is in the Stellenbosch district, between the Helderberg and Stellenbosch Mountains, and the Jonkershoek Valley.

The catchment of the Lourens River is in the Helderberg region. It is the region's largest river. The source is in Diepgat Ravine, in the Hottentots Holland Mountains. It is joined by minor tributaries from Landdroskloof and Sneeukopkloof in its upper reaches. The river flows in a south-westerly direction between the Helderberg and Schapenberg, through Somerset West and Strand, to a small estuary on the coast of False Bay. Its overall length is about 20 kilometres.

The Soete River is a small river that may have originally been part of the Lourens River system, diverting floodwater through an alternative route to the bay.

Sir Lowry's River drains the south side of Schapenberg and the west side of the Hottentots Holland south of Schapenberg. It enters the bay in Gordon's Bay.

The Steenbras River catchment is to the east of the Hottentots Holland mountains, and almost all of its water is retained by the upper and lower Steenbras Dams, which are a significant part of the municipal water supply to the City of Cape Town. Steenbras River mouth is south of Gordon's Bay.

The Rooiels River enters False Bay at Rooiels Beach. It drains a small catchment area in a nature reserve in the mountains of the southwest of the Overberg district.

Water quality

The nutrient contribution to False Bay surface waters from upwelling appears to exceed that from terrestrial sources via runoff and groundwater seepage. Still, pollutants from terrestrial sources can persist and adversely affect coastal ecosystems and recreational activities. Mixing with offshore water has a significant effect on surf zone and inshore water quality. The effects of microbial processes on inshore water quality and the relative contribution of anthropogenic nutrient sources remain unknown but are likely to be increasing.

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