After the strongest hurricane ever hits, it's natural to ask what happened.

What made this storm so strong?
Climatologists have ideas on the subject. Eli Rabbet looks at a graph from the NOAA Environmental Visulaization Lab. Darkness indicates warmth in the ocean, fuel for a potential hurricane.

Here's the commentary from the lab at the time:
The intensification of Super Typhoon Haiyan is being fueled by "ideal" environmental conditions – namely low wind shear and warm ocean temperatures. Maximum sustained winds are currently at 195 mph, well above the Category 5 classification used for Atlantic and East Pacific hurricanes. Plotted here is the average Tropical Cyclone Heat Potential product for October 28 – November 3, 2013, taken directly from NOAA View. This dataset, developed by NOAA/AOML, shows the total amount of heat energy available for the storm to absorb, not just on the surface, but integrated through the water column. Deeper, warmer pools of water are colored purple, though any region colored from pink to purple has sufficient energy to fuel storm intensification. The dotted line represents the best-track and forecast data as of 16:00 UTC on November 7, 2013.
Greg Laden, of Science Blogs, has a fine-grained description of the heat to energy transfer:
Warmer seas can make bigger or stronger storms, and as the storm passes over the ocean, the temperature of the sea surface has a strong influence on whether the storm increases or decreases in strength . As the storm moves over the sea, the interface between the windy storm and the roiling ocean becomes something of a mess, as though the surface of the ocean was in a blender, and there is a lot of exchange of heat across that interface. Also, deeper, cooler water is mixed with warmer surface water. A powerful storm moving across the ocean will leave in its wake a strip of cooler water.
Another way to look at heat content in the ocean is to look a chart for relative sea level, because, counter-intuitively, sea level is not exactly uniform the globe over.
Warmer regions tend to be elevated, and as a recent IPCC chart and discussion indicate, the waters near the Philippines are the warmest on the planet.

Jeff Masters describes what happened:
A remarkable warming of the sub-surface Pacific waters east of the Philippines in recent decades, due to a shift in atmospheric circulation patterns and ocean currents that began in the early 1990s, could be responsible for the rapid intensification of Super Typhoon Haiyan. Hurricanes are heat engines, which means they take heat energy out of the ocean, and convert it to kinetic energy in the form of wind. It's well-known that tropical cyclones need surface water temperatures of at least 26.5°C (80°F) to maintain themselves, and that the warmer the water, and the deeper the warm water is, the stronger the storm can get. Deep warm water is important, since as a tropical cyclone tracks over the ocean, it stirs up cooler water from the depths, potentially reducing the intensity of the storm. When both Hurricane Katrina and Hurricane Rita exploded into Category 5 hurricanes as they crossed over a warm eddy in the Gulf of Mexico with a lot of deep, warm water, the concept of the total heat energy available to fuel a hurricane–the Tropical Cyclone Heat Potential (TCHP)–became one that gained wide recognition. The Pacific Ocean east of the Philippines has the largest area of deep, warm water of anywhere on Earth, and these waters have historically fueled the highest incidence of Category 5 storms of anywhere on the planet. Super Typhoon Haiyan tracked over surface waters that were of near-average warmth, 29.5 – 30.5°C (85 – 87°F.) However, the waters at a depth of 100 meters (328 feet) beneath Haiyan during its rapid intensification phase were a huge 4 – 5°C (7 – 9°F) above average, judging by an analysis of October average ocean temperatures from the Japan Meteorological Agency (Figure 1.) As the typhoon stirred this unusually warm water to the surface, the storm was able to feed off the heat, allowing Haiyan to intensify into one of the strongest tropical cyclones ever observed.
Masters then adds a phenomenal plot from a Japanese meteorological agency that shows how closely the monster storm lined up with the warmest waters. Click if you want it bigger and clearer.

Figure 1. Departure of temperature from average at a depth of 100 meters in the West Pacific Ocean during October 2013, compared to a 1986 – 2008 average. The track and intensity of Super Typhoon Haiyan are overlaid. Haiyan passed directly over large areas of sub-surface water that were 4 – 5°C above average in temperature, which likely contributed to the storm's explosive deepening. Image credit: Japan Meteorological Agency.
As Kerry Emmanuel, of M.I.T., the leading expert on these storms, put it this week in the NYTimes:
//platform.twitter.com/widgets.js