2 Surface Temperature (AZMP)
Data Type: Tabular Data
Spatial Scope: Scotian Shelf (4X, 4V, 4W)
Duration 1948-2024
Source: DFO Atlantic Zone Monitoring Program via azmpdata
2.1 Introduction to Indicator
AZMP Surface Temperature contains empirical temperature measurements at 0m depth, averaged across NAFO divisions (4V, 4X, 4W) and regional boundaries (Bay of Fundy + Gulf of Maine). Data from this indicator is not subdivided regionally, but see Chapter 1 for spatially-stratified surface temperature data.
Sea surface temperature is influenced by a variety of conditions spanning multiple spatial and temporal scales. In this region, long-term trends in SST are consistent with expectations of anthropogenic climate change (Greenan et al. 2019). At the same time, decadal-to-interannual regional SST trends are influenced by atmospheric indicators like those described in this book, and short-term local values can be influenced by many oceanographic and climate factors, such as freshwater input, ocean currents, and weather events.
2.2 View Data
library(plotly)
plotly_df <- data@data %>%
mutate(
smooth_10yr = zoo::rollapply(mean_value, mean, width = 10, partial = TRUE),
overall_mean = mean(mean_value))
p <- plot_ly(plotly_df, x = ~year) %>%
add_lines(y = ~mean_value,
name = "Annual Mean",
line = list(color = "grey"),
hovertemplate = "Monthly anomaly: %{y:.2f}<extra></extra>"
) %>%
add_lines(y = ~smooth_10yr,
name = "10-yr Smooth",
line = list(color = "blue", 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 = "AZMP Surface Temperature for Scotian Shelf (4X, 4V, 4W)<br><sup>Source: DFO Atlantic Zone Monitoring Program via azmpdata</sup>",
xaxis = list(title = "Year"),
yaxis = list(title = "Surface Temperature (°C)",
fixedrange = TRUE),
hovermode = "x unified",
margin = list( t = 80)
) %>%
config(displayModeBar = FALSE)
pFigure 2.1: AZMP Surface Temperature in Scotian Shelf; 1948-2024
2.3 Summary and Trends
Trend and summary values are automatically generated; data were last updated on marea package install on 2026-02-10
As of the most recent data entry in 2024, the surface temperature value is 9.67 °C, which is high among values in the timeseries. Surface temperature is currently above the long-term mean, and has been since 2012.
Surface temperature has followed an increasing trend in recent years (Fig. 2.1).
2.3.1 Summary Table
Summary values for the AZMP Surface Temperature in the Scotian Shelf region are shown below (Table 2.1)
| Metric | Value | Description |
|---|---|---|
| Most Recent Value (2024) | 9.67 | The most recent value is high within the timeseries, in the 96.1 percentile of all values. The most recent value is 1.51 above the long-term mean. |
| Recent Trend (2014 – 2024) | 0.032 per year | In the last ten years, azmp_surface_temperature has increased by 0.032 per year with a Nonsignificant trend (p > 0.1). |
| Overall Trend (1948 – 2024) | 0.019 per year | Since the beginning of the timeseries, azmp_surface_temperature has increased by 0.019 per year with a Very Strong trend (p < 0.01). |
| Timeseries Record High | 10.34 | The highest value in the timeseries was recorded on 2012, and was 2.18 higher than the overall timeseries mean. |
| Timeseries Record Low | 6.25 | The lowest value in the timeseries was recorded on 1985, and was 1.91 lower than the overall timeseries mean. |
2.4 Relevance to Research and Stock Assessments
Changes to sea surface temperature could have great impact on fisheries and stocks from both direct and indirect effects.
Sea surface temperatures can directly impact fisheries via changes to the distribution and phenology of key fisheries species (Hutchings et al. 2012). These changes are likely to result in the loss or decline of some commercially important species, but also the gain or increase of others. Atlantic Canada is projected to experience decreases in species and maximum catch in the Scotian Shelf and surrounding bioregions, but projected gains towards the Arctic (Cheung et al. 2010). These changes are consistent with expected poleward shifts if species track climatic envelopes towards the poles. Changes to surface temperature might also affect phenological processes of key species, including spawning times and predator/prey encounters.
Sea surface temperatures can also affect the physical and chemical properties of marine ecosystems, in turn, affecting species. Warming and freshening of surface waters can lead to increased stratification in coastal oceans, influencing primary productivity and nutrient cycling.
2.5 Variable Definitions
| variable | description | unit |
|---|---|---|
| year | Year of data observations | |
| region | Area over which observations were summarized (only one: scotian_shelf_box) |
|
| mean_value | Averaged surface temperature in a given year | °C |