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How We Got Here — The Science Behind Our Striper Migration Forecast

Every fall, striped bass that spent the summer in Massachusetts head south toward New York, New Jersey and the mid-Atlantic. Our fall-run forecast tries to tell you roughly when that push is getting started and roughly when it might reach your stretch of coast. This page explains where the numbers come from. It also separates what scientists have actually measured from the choices we made to build a forecast.

The short version

1. Where the 62°F number comes from

The main source is a University of Massachusetts Amherst–led acoustic tagging study in Plymouth, Kingston and Duxbury Bay, about 30 miles south of Boston (Hollema et al., 2017, Fisheries Research).

What that does and does not mean

2. Why we use the Boston buoy, and why that's our choice

The bay study measured water inside a shallow, sheltered estuary. We use NOAA buoy 44013, which sits in open water about 16 nautical miles east of Boston. We picked it because it reports every hour and has a long public record.

Those are different environments. Shallow bays usually warm faster in summer and cool faster in fall than open water. So 62°F at the offshore buoy is not necessarily the same moment as 62°F inside Plymouth–Duxbury Bay. Using the buoy as a stand-in for the conditions the bay fish experienced is our modeling assumption, not a finding of the study.

We added the October 1 rule ourselves for two reasons. It lines up with the day-length half of the study's result, and it keeps a short September cold snap or upwelling event from setting off the trigger too early. In 3 of the last 11 years (2017, 2020 and 2022), the buoy's 7-day average briefly dipped to 62°F or lower in late September.

3. Eleven years of Boston buoy data

We pulled NOAA's hourly water temperatures for station 44013 from 2015 through 2025, averaged them by day, and then took a trailing 7-day average. For each year, the table shows the first day on or after October 1 when that 7-day average was 62°F or cooler.

Median trigger date: October 12. Range: October 1 to October 22.

Left: 7-day average water temperature at NOAA buoy 44013 from September through November, 2015–2025, shown as a shaded range with the median year and 2025. A dashed line marks 62°F. Right: bar chart of each year's trigger date, from October 1 (2022) to October 22 (2021), median October 12.
Year Trigger date (7-day avg ≤ 62°F, on/after Oct 1) 7-day avg on Oct 1
2015 Oct 3 62.7°F
2016 Oct 3 62.5°F
2017 Oct 14 63.5°F
2018 Oct 14 64.0°F
2019 Oct 6 64.2°F
2020 Oct 5 62.5°F
2021 Oct 22 63.9°F
2022 Oct 1 60.7°F (already below)
2023 Oct 13 62.7°F
2024 Oct 12 62.7°F
2025 Oct 13 64.4°F

For comparison, the same buoy didn't reach a 7-day average of 52°F until November 15–30 in any of those years. An older trigger based on "low-50s" water would therefore have fired well after most tagged Massachusetts fish had already left.

4. What other tagging studies show

Several other peer-reviewed studies tracked striped bass leaving Massachusetts. They agree on the broad pattern, and they also show how much individual fish differ.

5. What we know about timing in New Jersey

The direct New Jersey evidence is thinner, and we want to be upfront about that.

Those New Jersey studies cover estuary fish, some of which may be local. They don't directly measure when Massachusetts fish pass a particular New Jersey beach. We haven't found a peer-reviewed study that gives a typical arrival date for migrating Massachusetts striped bass along the New Jersey ocean beaches.

6. Our 15-mile-per-day pace: a modeling assumption

The 15-mile-per-day pace is a forecasting assumption that we set. It is not a measured swimming speed, and no study has validated it.

Here's how it compares with what has been measured:

So 15 miles per day is meant to follow the leading edge of the run, the point where good numbers of fish first show up. It doesn't describe how fast any one fish swims. We'll adjust it if better evidence comes in.

7. Limits of this forecast

Sources

  1. Hollema, H. M., Kneebone, J., McCormick, S. D., Skomal, G. B., & Danylchuk, A. J. (2017). Movement patterns of striped bass (Morone saxatilis) in a tidal coastal embayment in New England. Fisheries Research, 187, 168–177. https://doi.org/10.1016/j.fishres.2016.11.006
  2. Kneebone, J., Hoffman, W. S., Dean, M. J., Fox, D. A., & Armstrong, M. P. (2014). Movement patterns and stock composition of adult striped bass tagged in Massachusetts coastal waters. Transactions of the American Fisheries Society, 143(5), 1115–1129. https://doi.org/10.1080/00028487.2014.889752
  3. Mather, M. E., Finn, J. T., Pautzke, S. M., Fox, D. A., Savoy, T., Brundage, H. M., Deegan, L. A., & Muth, R. M. (2010). Diversity in destinations, routes and timing of small adult and sub-adult striped bass Morone saxatilis on their southward autumn migration. Journal of Fish Biology, 77(10), 2326–2337. https://pubs.usgs.gov/publication/70037711 (DOI: https://doi.org/10.1111/j.1095-8649.2010.02811.x)
  4. Secor, D. H., O'Brien, M. H. P., Gahagan, B. I., Fox, D. A., Higgs, A. L., & Best, J. E. (2020). Multiple spawning run contingents and population consequences in migratory striped bass Morone saxatilis. PLOS ONE, 15(11), e0242797. https://doi.org/10.1371/journal.pone.0242797
  5. Secor, D. H., O'Brien, M. H. P., Gahagan, B. I., Watterson, J. C., & Fox, D. A. (2020). Differential migration in Chesapeake Bay striped bass. PLOS ONE, 15(5), e0233103. https://doi.org/10.1371/journal.pone.0233103
  6. Able, K. W., & Grothues, T. M. (2007). Diversity of estuarine movements of striped bass (Morone saxatilis): a synoptic examination of an estuarine system in southern New Jersey. Fishery Bulletin, 105(3), 426–435. https://spo.nmfs.noaa.gov/sites/default/files/pdf-content/2007/1053/able.pdf
  7. Ng, C. L., Able, K. W., & Grothues, T. M. (2007). Habitat use, site fidelity, and movement of adult striped bass in a southern New Jersey estuary based on mobile acoustic telemetry. Transactions of the American Fisheries Society, 136(5), 1344–1355. https://scholarship.libraries.rutgers.edu/esploro/outputs/journalArticle/Habitat-Use-Site-Fidelity-and-Movement/991031654602604646
  8. NOAA National Data Buoy Center. Station 44013, Boston (16 NM east of Boston). Station page: https://www.ndbc.noaa.gov/station_page.php?station=44013 · Historical data: https://www.ndbc.noaa.gov/station_history.php?station=44013 · Annual files used: https://www.ndbc.noaa.gov/data/historical/stdmet/44013h2015.txt.gz through 44013h2025.txt.gz

Methods note: Water temperature (WTMP, °C) from NDBC historical standard meteorological files, missing values (99/999) removed, daily means converted to °F, trailing 7-day mean requiring at least 5 days of data. Route distances are approximate straight-line sums between coastal waypoints (Boston, Cape Cod Canal, Point Judith, Montauk, Fire Island, Sandy Hook, Barnegat, Atlantic City, Cape May), not measured fish paths.