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Main articles: PortMiami Tunnel and PortMiami Deep Dredge Project The Gulf Stream and its northern extension towards Europe the North Atlantic Drift is thought to have at least some influence on climate for example the Gulf Stream helps moderate winter temperatures along the coastline of southeastern North America keeping it warmer in winter along the coast than inland areas the Gulf Stream also keeps extreme temperatures from occurring on the Florida Peninsula in the higher latitudes the North Atlantic Drift warms the atmosphere over the oceans keeping the British Isles and north-western Europe mild and cloudy and not severely cold in winter like other locations at the same high latitude the cold water currents contribute to heavy fog off the coast of eastern Canada (the Grand Banks of Newfoundland area) and Africa's north-western coast in general winds transport moisture and air over land areas. Adrienne Arsht Center for the Performing Arts the second-largest performing arts center in the United States. . The FIU College of Law was ranked 5th in 2014 in bar passing rates in the state of Florida and 1st in the MPRE. .

As of 2010 the population of Downtown Miami was 65,696 people with a population density of 27,487 per square mile in the 2010 US Census the racial makeup of Downtown was 57.6% Hispanic of any race 30.8% White (non-Hispanic) 7.2% Black and 2.9% Asian the zip codes for Brickell include 33129 33130 and 33131 the area covers 1.084 square miles (2.81 km2), 2009 Census projections indicate that the area's residential base has increased from 40,000 to 71,000 since 2000 with an expected Downtown population of 85,000 by 2014 as of 2006 189,164 residents live in the immediate Downtown/Brickell area, Education households income and poverty. (18.6) 59.5 Map displaying a looping line with arrows indicating that water flows eastward in the far Southern ocean angling north east of Australia turning sough after passing Alaska then crossing the mid-Pacific to flow north of Australia continuing west below Africa then turning northwest until reaching eastern Canada then angling east to southern Europe then finally turning south just below Greenland and flowing down the Americas' eastern coast and resuming its flow eastward to complete the circle.