Table 1 Coastal locations of (in situ) water temperature measurements used in this study. The sites were selected to represent the broad range of Patella vulgata’s southern distribution. Temperatures were recorded by Maxim DS1922 iButton loggers deployed in the intertidal at 0–1 m below Mean Sea Level (MSL) at a particular frequency (in minutes, tx). Daily values were obtained by averaging data collected by one of multiple sensors (N loggers). These in situ measurements were used to calculate a Thermal Upwelling Index (UI, in °C) for each location, defined as the magnitude of the cold anomaly (i.e. cold bias) between upwelled coastal waters and the warmer offshore waters47,66. Manufacturer reported logger accuracy and resolution for the iButton loggers were both 0.50 °C.

From: Coastal upwelling generates cryptic temperature refugia

Country

Location

Lat (degrees)

Lon (degrees)

tx (min)

N loggers

UI (°C)

Classification

Scotland

South Cairn

54.97

− 5.18

60

18

0.8

Weak upwelling

Ireland

Emlagh

53.75

− 9.91

60

18

0.4

No upwelling

Wales

Isle of Anglesey

53.32

− 4.66

60

18

0.4

No upwelling

Ireland

Minard Castle

52.13

− 10.11

60

18

0.3

No upwelling

England

Wembury

50.31

− 4.11

60

18

0.6

Weak upwelling

France

Landunvez

48.54

− 4.75

60

18

1.0

Weak upwelling

France

Le Croisic

47.29

− 2.54

60

18

0.3

No upwelling

France

Royan

45.61

− 1.03

60

18

0.2

No upwelling

France

Biarritz

43.48

− 1.56

60

18

0.2

No upwelling

Spain

San Vicente de la Barquera

43.41

− 4.44

60

18

0.6

Weak upwelling

Spain

La Caridad

43.57

− 6.83

60

18

0.6

Weak upwelling

Spain

Cabo Tourinan

43.04

− 9.29

60

18

2.0

Strong upwelling

Portugal

Modelo

41.84

− 8.87

60

18

2.1

Strong upwelling

Portugal

São Lourenço

39.01

− 9.42

60

18

2.7

Strong upwelling

Portugal

Alteirinhos

37.52

− 8.79

60

18

1.7

Strong upwelling

Portugal

Evaristo

37.07

− 8.30

60

18

0.9

Weak upwelling