Gibraltar crossing.

 Gibraltar crossing.

As I have posted extensively building massive urban complexes upon massive secure concrete hulled barges is plausible for providing human residency on the ocean. Bluntly put, the bigger the safer.

My initial considerations viewed the Salish SEA as ideal along with the northern Adriatic.  both these are seriously attractive as housing destinations.  Do understand that these are housing builds providing the actual capital.  Road, Rail, massive factory space and massive greenhouse space are all secondary to the primary build.

Those are the super safe and best possible economic models.  Many others exist of course even with geographic protection, but often without adjacent real estate demand.  Initially those economic issues will matter most.  In Vancouver's case, it becomes plausible to build out a ten million population on the Salish sea and also connect properly to Vancouver Island.

Again, you have to imagine building a potential kilometer by kilometer floating barge that once anchored never leaves.  On this giant barge you then build condo towers fifteen stories tall along the edges at least and however you design elsewhere.  The edges matter because that is where you can provide design strength.

Again, the only external stressor will be moderate wave activity overcome easily by operational size and mass.  There is zero earthquake risk which is a major current cost for all such constructs, particularly where we mostly build along the Pacific Rim.

My take home is that building big enough will easily provide at sea conventional housing on a barge like foundation whose horizontal component can provide roadbeds and even factory and greenhouse space.  Better yet, big enough opens the door to even deep sea complexes even though no one needs to start there because we all want initially road and rail access.

Now this brings us back to Gibraltar which is just too large and deep to support bridging.  Here a floating urban complex with a  full rail and super highway complex though its center is a plausible build again with the housing at least paying for the foundation barge and housing.  Better yet ship channels can be provided at either end as well where bridging should be possible.

The foundation barges can be a mile long and a quarter mile wide as a first estimate.  Recall bigger is safer.  The only other obvious issue will be fouling which since no movement is necessary, will self correct by ultimately sheering off naturally. 

This would be an exciting build and captures everyone imagination while driving the economies on both sides of the strait.

This is also likely the most studied body of water on the planet.

Navigating the Strait of Gibraltar Tides

Posted by Penny Haire on 27 August 2020 3:10:10 PM

Suppose you're familiar with oceanography and some of the more treacherous shipping routes of the world. In that case, you'll know about the challenges for the shipping industry that the Strait of Gibraltar poses. This narrow passage that connects the Atlantic Ocean to the Mediterranean Sea has many elements that contribute to the complexity of tides and currents in this area, and this article explores how it all works.

From the rapid evaporation of water that exceeds the influx of water from rivers and rain to the layers of seawater, each of a different density and salinity, there are several ever-changing elements to be aware of when transiting the Strait of Gibraltar.

Here's an outline of just how and why these infamous straits are so complex to navigate.

The Density of Seawater in the Gibraltar Strait

One of the singular features of the Strait of Gibraltar is the Mediterranean inflow and outflow, which consists of layers of water that have different salinity (levels of salt).

The water in the Atlantic is less salty and less dense than water in the Mediterranean, and it flows eastwards into the Mediterranean through the Straits as a surface layer, about 125m deep with a speed of two to three knots.

In contrast, there is a westward outflow of heavier, colder, and more salty water, which works its way out into the Atlantic. The tidal flow will either speed up or slow down the eastern flowing current, depending on the phase of the tide.

An Ever-Evaporating Sea

A very distinctive feature of the Strait of Gibraltar is it's continually evaporating body of water. The Mediterranean Sea loses nearly a meter of vertical water height every year.

Around 7 million years ago, the general shape of the Mediterranean basis was nearly the same as today. Due to the movement of tectonic plates, the inflow of water from the ocean to the sea was cut off, leaving the area to evaporate completely. However, around 5.3 million years ago, the tectonic plates moved again, opening the Strait and allowing an immense amount of water to flow from the ocean, filling the Mediterranean basin once again.

This evaporation is still occurring today, and it's estimated that were the Strait closed today at our current higher sea level, the basin would evaporate once again.

Counter Currents and Internal Waves

To add another challenging piece to the tidal puzzle that makes up the Strait of Gibraltar, close to the African continent, there is often a narrow counter current of two knots that interacts with the Camarinal Still (the shallowest part of the Strait) and causes internal waves. As noted by NASA;

"The waves are generated as a diurnal tidal pulse flows over the shallow Camarinal Sill at Gibraltar. The waves flow eastward, refract around coastal features; can be traced for as much as 150 km, and sometimes create interference patterns with refracted waves." - Earth Observatory, NASA

These internal waves are a vertical motion between the two layers and can have a displacement sometimes exceeding 100m with a wavelength of two to four km. They're so distinct as a surface wave pattern that sunlight is deferentially scattered off the water surface and the waves can be observed by astronauts in space!

You can see exactly how this looks in the video below.

The Alboran Gyre

As the upper-level flow pours into the Mediterranean, the Coriolis force (an effect of the earth's rotation) causes it to form a large clockwise eddy (gyre) off the North African coast called the Alboran Gyre. A smaller weak anti-clockwise eddy forms to the North. Countercurrents (westward flows) can be seen close inshore along both shores, particularly near headlands that project into the current.

The western end of the Mediterranean, the Alboran Sea, is the habitat for the largest population of bottlenose dolphins in the western Mediterranean, is home to the last population of harbour porpoises in the Mediterranean, and is the most important feeding ground for loggerhead sea turtles in Europe.

A layer of outward-flowing dense water stays deep after exiting the Mediterranean and forms a ribbon extending along the Spanish and Portuguese coasts at about 1000m depth. It splits into two at Cape St Vincent, with one branch going west and the other branch going North. Evidence of this flow is seen as far north as the Greenland-Scotland sill.

Amazingly, the westward flowing Mediterranean water reaches the American continent and travels south to Antarctica and the Weddell Sea.

Modelling the Strait of Gibraltar

Over 100,000 ships transit through Gibraltar every year for commercial purposes, so modelling of the complexity of the Strait is key for safe passage.