Forecast and Analysis

Traffic Report, Northeastern US: 13-20 April 2016

Andrew Farnsworth The Cornell Lab Apr 22, 2016

Welcome to this installment of BirdCast Traffic Reports, posts describing northeastern US nocturnal bird migration traffic rates, as calculated from a completely automated pipeline of algorithms. The images you see in Traffic Reports present the migration traffic rate (MTR), direction of bird movement, and speed of bird movement. See our first report or scientific paper (currently a preprint) for more information about the calculations and algorithms we use.

13-20 April was a period with substantially more exciting movements than previous weeks in the northeastern US. Substantial movements occurred on several nights, most notably 14-16 April. Inland flights dominated these movements, particularly in Ft. Drum, Binghamton, Buffalo, and Albany, NY, and State College, PA. Remember, traffic, specifically migration traffic rate in our case, is defined as the number of birds from 0-3,000 meters above radar stations moving hourly over a 1 km line drawn on the ground.

_summary_2016-04-14_2016-04-20_

 

Nightly migration loops

April saw an unseasonable blast of cool in the region. Lackluster movements characterized the migration scene in our previous report, but changes are afoot, clearly, in the current report. 14-16 April highlighted the peaks of movements from a regional perspective. In particular, 14 April saw the first substantial and widespread flight of the spring, with many inland stations participating. Most birds were moving in a northerly or northeasterly direction, with the largest flights over central New York. Note that coastal locations generally did not participate in this suite of movements.

Similarly, 16 April saw similarly widespread flights, but with a more northerly distribution. Most movements were primarily oriented toward the northeast. Note, also, that Maine experienced flights part of the movements in the northern half of the region.

Coastal flights were generally muted during this period because of persistent easterly flow associated with a strong blocking high pressure center in the North Atlantic. And remember in both of these cases, our model is not perfect, and some of these detections may be erroneous classifications of precipitation as birds.

For more detailed accounting of what species were migrating during this period, please visit our regional migration analyses (herehere and here) for the Upper Midwest and Northeast in which we (as humans not just algorithms!) describe and interpret movements in greater detail.

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