Such is the nature of the tropics -- and specifically, of the Inter-Tropical Convergence Zone. The ITCZ, as it is called (when it is not called the doldrums, that is!), shows up on a satellite images as a band of clouds that encircles the globe near the equator. This band of clouds can be thick and solid, extending hundreds of miles. Or, it may be broken into smaller lines of clouds with sunny skies in between.
The Intertropical Convergenze Zone (ITCZ) -- image from http://radar.weather.gov/jetstream/tropics/itcz.htm.
Large-scale movement of the ITCZ occurs seasonally. It is farther north in June, July and August; farther south in January, February, and March. This seasonal movement is what causes the rainy seasons in the tropics. But, although the large-scale movements of the ITCZ occur on seasonal timescales, the ITCZ also moves from day to day, albeit over much shorter distances.
The map below shows the position of the ITCZ today (March 4th) and two days ago. As you can see from our cruise track, we were just south the line marking the center of the zone of ITCZ cloudiness (the "axis" of the ITCZ) at the start of our work, but are now north of the axis.
Early March positions of the ITCZ relative to our cruise track (ITCZ positions from the NWS
tropical weather discussions web pages: http://www.weather.gov/view/national.php?prodtype=tropical).
So, although yesterday morning I managed to get a solid hour and a half of reading time out in the sunshine, this morning has been socked in with heavy clouds and squalls. Such is life in the tropics!
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