10 North Atlantic Oscillation Index

Data Type: Tabular Data

Spatial Scope: North Atlantic

Duration 1951-2024

Source: NOAA NCEP via azmpdata; https://www.ncei.noaa.gov/access/monitoring/nao/

10.1 Introduction to Indicator

The North Atlantic Oscillation (NAO) index is defined as the winter (December, January, February, March) 500 mb pressure Principal Component Analysis which is representative of the difference between the Icelandic low and Azores high.

The NAO in linked to several weather and climate phenomena in the North Atlantic, including speed and direction of westerly winds, storm activity, and precipitation patterns from the North American Eastern Seaboard to Europe and Siberia (Hurrell et al. 2003).

In Canada, high NAO values are typically associated with cold air and sea temperatures off the Eastern coast, northwest wind patterns, and ice in the Laborador and Newfoundland shelves, whereas low NAO values are associated with the opposite (Layton et al. 2025).

10.2 View Data

library(plotly)
plotly_df <- data@data %>%
  mutate(smooth_10yr = zoo::rollapply(anomaly_value, mean, width = 10, partial = TRUE),
         overall_mean = mean(anomaly_value))

p <- plot_ly(plotly_df, x = ~year) %>%
  add_lines(y = ~anomaly_value,
            name = "Yearly Anomaly",
            line = list(color = "lightgrey"),
            hovertemplate = "Monthly anomaly: %{y:.2f}<extra></extra>"
           ) %>%
  add_lines(y = ~smooth_10yr,
            name = "10-yr Smooth",
            line = list(color = "red", width = 2),
            hovertemplate = "10-yr smoothed: %{y:.2f}<extra></extra>",
           ) %>%
    add_lines(y = ~overall_mean,
            name = "Overall Mean",
            line = list(color = "black", width = 2, dash = "dash"),
            hovertemplate = "Overall Mean: %{y:.2f}<extra></extra>",
           ) %>%
  layout(
    title = "North Atlantic Oscillation Index for North Atlantic",
    xaxis = list(title = "Date"),
    yaxis = list(title = "NAO Index",
                 fixedrange = TRUE),
    hovermode = "x unified",
    margin = list( t = 80)
    
  ) %>%
  config(displayModeBar = FALSE) 

p

Figure 10.1: NAO Index Value; 1951-2024

10.4 Relevance to Research and Stock Assessments

The NAO is closely linked to ecosystem and fisheries dynamics in the North Altantic, with variable impacts on the Northeast and Northwest.

In Canada, negative NAO values are associated with favorable conditions for important fisheries such as cod and other groundfish, whereas positive NAO values are associated with unfavorable conditions. Positiove NAO values drive stronger northwesterly winds off Eastern Canada, as well as colder sea temperatures, which are negatively associated with cod recruitment (Mann and Drinkwater 1994). Positive NAO values in the 1980s and 1990s are hypothesized to have contributed (along with overfishing) to the decline in cod in Eastern Canada during that time (Parsons and Lear 2001).

Conversely, cold conditions during positive NAO phases are favorable for recruitment of snow crabs on the Newfoundland and Labrador shelves. Following favorable early-life conditions, NAO values are correlated with exploitable biomass of snow crabs on a 6-8 year lag (Fisheries and Oceans Canada (DFO) 2022).

10.5 Variable Definitions

Table 10.2: Column names and definitions in the NAO dataset.
variable description unit
year year of modeled value
anomaly_value NAO anomaly

10.6 Additional Data

No additional data for NAO.

10.7 Get the Data

library(marea)
data('nao')
plot(nao)

References

Fisheries and Oceans Canada (DFO). 2022. “Assessment of Newfoundland and Labrador (Divisions 2HJ3KLNOP4R) Snow Crab.” 2022/012. DFO Can. Sci. Advis. Sec. Sci. Advis. Rep. Canadian Science Advisory Secretariat, Fisheries; Oceans Canada. https://waves-vagues.dfo-mpo.gc.ca/library-bibliotheque/41058781.pdf.
Hurrell, James W, Yochanan Kushnir, Geir Ottersen, and Martin Visbeck. 2003. “An Overview of the North Atlantic Oscillation.” Geophysical Monograph-American Geophysical Union 134: 1–36.
Layton, C, D Brickman, B Greenan, P Galbraith, and JL Shaw. 2025. “Physical Oceanographic Conditions on the Scotian Shelf and in the Gulf of Maine During 2024.” Dartmouth, Nova Scotia: Fisheries; Oceans Canada, Bedford Institute of Oceanography. https://publications.gc.ca/site/eng/9.953493/publication.html.
Mann, KH, and KF Drinkwater. 1994. “Environmental Influences on Fish and Shellfish Production in the Northwest Atlantic.” Environmental Reviews 2 (1): 16–32.
Parsons, LS, and WH Lear. 2001. “Climate Variability and Marine Ecosystem Impacts: A North Atlantic Perspective.” Progress in Oceanography 49 (1-4): 167–88.