| Year |
Bottom trawl
|
Long lines
|
Other gears
|
Total
|
|||
|---|---|---|---|---|---|---|---|
| Vessel (number) | Catch (tonnes) | Vessel (number) | Catch (tonnes) | Vessel (number) | Catch (tonnes) | Catch (tonnes) | |
| 2000 | 183 | 103 558 | 530 | 49 946 | 827 | 17 623 | 186 057 |
| 2001 | 160 | 99 071 | 515 | 47 172 | 766 | 17 002 | 180 260 |
| 2002 | 155 | 87 885 | 450 | 42 405 | 724 | 19 305 | 163 179 |
| 2003 | 147 | 88 422 | 461 | 44 654 | 721 | 16 026 | 162 477 |
| 2004 | 135 | 95 769 | 470 | 57 397 | 722 | 14 840 | 182 234 |
| 2005 | 134 | 84 018 | 463 | 69 444 | 604 | 8 106 | 174 338 |
| 2006 | 126 | 82 417 | 447 | 71 037 | 509 | 5 859 | 169 671 |
| 2007 | 123 | 71 499 | 425 | 58 943 | 473 | 4 397 | 143 550 |
| 2008 | 113 | 58 172 | 370 | 53 843 | 427 | 4 151 | 124 607 |
| 2009 | 113 | 79 667 | 336 | 61 005 | 798 | 8 190 | 159 232 |
| 2010 | 111 | 75 609 | 286 | 57 491 | 1 008 | 9 372 | 150 768 |
| 2011 | 110 | 73 538 | 290 | 57 711 | 1 061 | 12 665 | 153 020 |
| 2012 | 118 | 85 265 | 305 | 67 777 | 1 099 | 13 417 | 176 448 |
| 2013 | 110 | 101 453 | 297 | 74 835 | 1 054 | 15 237 | 201 617 |
| 2014 | 110 | 95 830 | 292 | 77 807 | 1 012 | 16 355 | 200 399 |
| 2015 | 103 | 103 530 | 266 | 79 244 | 943 | 13 957 | 208 669 |
| 2016 | 99 | 111 016 | 246 | 84 509 | 956 | 15 299 | 226 754 |
| 2017 | 94 | 117 891 | 221 | 75 244 | 832 | 14 945 | 223 478 |
| 2018 | 83 | 135 030 | 201 | 78 316 | 813 | 16 221 | 245 385 |
| 2019 | 81 | 135 661 | 190 | 78 326 | 794 | 13 592 | 241 760 |
| 2020 | 81 | 146 788 | 158 | 68 103 | 839 | 15 884 | 246 973 |
| 2021 | 87 | 140 773 | 146 | 69 632 | 841 | 16 014 | 244 114 |
| 2022 | 83 | 124 950 | 121 | 62 795 | 850 | 15 172 | 219 413 |
| 2023 | 81 | 117 580 | 99 | 54 527 | 866 | 13 389 | 201 511 |
| 2024 | 79 | 123 832 | 90 | 49 139 | 849 | 15 238 | 203 602 |
Key signals
Survey biomass increased steadily from 2008 to 2012, after which high but variable levels were observed in both the spring and autumn surveys. Since 2012, discrepancies have emerged between the two surveys: the spring survey shows a stronger upward trend, while the autumn survey indicates more stable or modest increases. The most recent spring survey, however, shows a marked decline in biomass.
Recruitment (age 3) was substantially higher prior to 1985 but has remained relatively stable over the past decade. The year classes 2020–2022, recruiting in 2023–2025, are at or below the long-term average, suggesting a likely decline in reference biomass as these cohorts reach age 4. Several of these cohorts also exhibit low stock and catch weights at ages 4–7, which make up the bulk of the reference biomass.
Harvest rates exceeded the management target of 0.2 prior to 2022 but have since fluctuated around the target level.
Length distributions have been stable over the past decade, reflecting periodic recruitment and a broad range of sizes in the population. However, the abundance of fish in the <50 cm is lower than in most recent years, supporting expectations of reduced biomass in the near term.
Spawning stock biomass (SSB) peaked in 2018–2019, reaching its highest level since before 1970. Although SSB is now declining, it remains relatively high compared to most levels observed since 1980.
General information
Cod (Gadus morhua) is widely distributed in Icelandic waters, with the highest abundance found on the northwestern, northern, and northeastern parts of the continental shelf. As a demersal species, cod occupies a wide depth range, typically from a few meters down to 600 m, and occasionally deeper. Adult cod are not strongly selective regarding bottom substrate and can be found on a variety of seabed types. In contrast, juveniles prefer moderately sheltered, shallow habitats such as kelp forests and seagrass beds. Cod thrive in sea temperatures around 4–7°C, although they are frequently caught in waters below 2°C.
Cod spawn around the Icelandic coastline in distinct regional spawning components. The primary spawning areas are located in the south, southwest, and west, where spawning begins early in spring (March–April) in warmer waters. In recent years, spawning activity has shifted westward (Jónsdóttir et al. (2025)). Historically, spawning occurred later in the colder northern waters, but the spawning period there has advanced considerably. Pelagic eggs and larvae drift predominantly northward and eastward, following a clockwise pattern to nursery areas in the north and northeast. Adult cod undertake feeding migrations to deeper waters in the northwest and southeast, although some remain in shallow areas to feed. Cod is Iceland’s most significant groundfish species in terms of commercial importance.
Fishery
Landing trends
Cod landings from Iceland waters have been consistently high since records began in 1903, typically ranging from 300 to 450 thousand tonnes prior to World War II and again between 1950 and 1990 (Figure 1). During the World Wars, foreign fleets ceased operations in Icelandic waters, while Icelandic catches remained stable. Throughout much of the 20th century, foreign vessels accounted for a significant share of the catch until Iceland extended its Exclusive Economic Zone (EEZ) to 200 miles in 1976.
Catch levels have largely been shaped by stock productivity, influenced by both recruitment and immigration from Greenland. Significant migration events from Greenland to Iceland occurred in the 1930s and in 1953. A reduction in fishing effort during World War II also contributed to stock rebuilding.
Between 1955 and 1990, landings gradually declined. From 1992 onward, average catches have been around 219 thousand tonnes (range: 148–270 thousand tonnes). In 2025, landings totaled 218833 tonnes. A small share of this (2408 tonnes) was landed by Norwegian and Faroese vessels under bilateral agreements (Figure 1).
Historically, bottom trawl and gillnets were the primary gear types (Figure 2). Bottom trawl has consistently made up at least 40% of catches, rising to about 55% in recent years, while gillnet use declined from 20% before 2001 to around 7% more recently. Most bottom trawl catches occur in the northwest, while gillnet catches have been concentrated in the south and west during spawning. The share of longline catches has increased over time, with large longline vessels with automatic baiting extending the fishery into deeper waters. Before 2003, longlines accounted for about 20% of catches; this rose to around 35% during 2005–2016. Demersal seines have contributed a steady 5–8% of total catches. In some regions, especially the northwest and southeast, cod aggregate in dense schools, allowing captains to quickly fill quotas, particularly prior to landing. Cod condition and size, along with proximity to landing ports, also influence fishing locations.
In 2025, bottom trawls accounted for more than half of total catches (57%), followed by longlines (22%), gillnets (7%), jiggers (7%), and demersal seines (7%). The largest proportion of the catches were taken from the western and northwestern regions, followed by the northeast and southwest. Catches occurred at similar depths as in previous years, although slightly shallower overall (Figure 2).
The depth distribution of the fishery has shown little change (Figure 3).
Due to its wide distribution, cod is fished across the Icelandic shelf using various gear types (Figure 4, Figure 5, Figure 6). Demersal trawl is the main fishing gear (Figure 4), with primary fishing areas located in deeper, colder waters offshore in the northwest, northeast, and east. Over recent years, trawl effort has increasingly concentrated in these hotspots.
Longlines account for the second-largest share of cod catches and are widely used around the shelf, with the lowest effort on the southern and southeastern coasts (Figure 5). The spatial pattern of longline catches has remained generally consistent, with periodic hotspots. Gillnets, demersal seines, and jiggers contribute smaller shares and primarily operate in shallower waters (Figure 6).
Since 2000, the share of cod catches from the northwestern area increased from about 35% to 40–50% in 2011–2024 (Figure 7 and Figure 8 ). In contrast, catches west of Iceland declined from 25–30% to just under 20%, and from the southeast, from 5–10% to below 5%. Other areas have remained stable, with the northeast contributing around 20% and the southwest about 10%.
The number of vessels accounting for 95% of annual cod landings declined from around 1000 to 750 during 1994–1999, despite a notable increase in total catch (Figure 9). Between 1999 and 2008, vessel numbers declined further to below 400, in line with reduced catches. After a temporary increase during 2009–2014, the number of vessels has since decreased to around 300. This trend is evident across all fleet segments (Table 1).
Catch per unit of effort from commercial fisheries
Catch per unit of effort (CPUE) data (Figure 10) indicate a steady increase since 1990 for the main gear types in hauls where cod accounts for more than 50% of the catch. Overall CPUE across all gears is among the highest on record. CPUE could not be estimated after 2021 due to missing effort data for several years.
Landings and discards
Landings data before 1982 (and foreign landings until 2005) are sourced from the ICES STATLANT database. Icelandic landings between 1982–1993 were collected by the Fisheries Association of Iceland, and from 1994 onward by the Directorate of Fisheries. Foreign landings were recorded by the Coast Guard before 2014 and by the Directorate thereafter.
Discarding is prohibited by law. Management measures, such as inter-species quota transfers and landing flexibility, discourage discarding. To help prevent high grading and quota mismatches, fisheries are permitted to land catches that are exempt from quota deductions, provided that the proceeds from their sale are transferred to a government-managed fund. More information is available at https://www.responsiblefisheries.is/seafood-industry/fisheries-management.
Data and sampling
Commercial data
Sampling coverage from commercial catches is generally good for the main gears (demersal seines, longlines, gillnets, bottom trawls), with broad spatial and seasonal representation (Figure 12, Figure 13).
Length compositions
The length distribution of landed cod has shifted toward larger fish over the past decade (Figure 14). Most length data come from bottom trawl, longline, gillnet, and demersal seine fleets (Table 2). Gear-specific sample sizes have varied with fleet composition.
| Year |
Bottom Trawl
|
Danish Seine
|
Gillnets
|
Long Line
|
||||
|---|---|---|---|---|---|---|---|---|
| Num. samples | Num. lengths | Num. samples | Num. lengths | Num. samples | Num. lengths | Num. samples | Num. lengths | |
| 2000 | 766 | 172 132 | 23 | 3 265 | 27 | 4 517 | 124 | 29 780 |
| 2001 | 1 131 | 170 398 | 79 | 13 660 | 541 | 39 836 | 281 | 39 915 |
| 2002 | 1 233 | 162 365 | 122 | 19 057 | 443 | 45 520 | 338 | 46 560 |
| 2003 | 1 131 | 114 366 | 73 | 13 283 | 512 | 32 729 | 444 | 67 124 |
| 2004 | 1 239 | 107 977 | 97 | 17 943 | 310 | 28 422 | 467 | 85 952 |
| 2005 | 1 092 | 101 166 | 298 | 18 050 | 267 | 37 554 | 549 | 108 597 |
| 2006 | 859 | 79 264 | 159 | 15 812 | 349 | 34 329 | 776 | 115 401 |
| 2007 | 946 | 75 259 | 416 | 16 252 | 304 | 24 024 | 498 | 96 662 |
| 2008 | 849 | 67 630 | 297 | 14 065 | 370 | 23 676 | 530 | 105 864 |
| 2009 | 884 | 76 100 | 216 | 15 306 | 205 | 25 436 | 420 | 86 909 |
| 2010 | 806 | 77 979 | 139 | 10 621 | 152 | 26 303 | 401 | 81 373 |
| 2011 | 596 | 64 643 | 86 | 6 604 | 162 | 29 203 | 280 | 55 614 |
| 2012 | 604 | 54 037 | 104 | 8 282 | 131 | 22 678 | 438 | 97 729 |
| 2013 | 659 | 73 853 | 50 | 2 196 | 25 | 3 532 | 393 | 83 001 |
| 2014 | 531 | 46 615 | 40 | 5 118 | 141 | 27 103 | 453 | 96 534 |
| 2015 | 554 | 65 641 | 47 | 5 880 | 56 | 5 860 | 376 | 83 342 |
| 2016 | 493 | 57 116 | 51 | 6 201 | 150 | 25 919 | 421 | 96 525 |
| 2017 | 518 | 67 512 | 61 | 7 073 | 47 | 7 149 | 368 | 77 691 |
| 2018 | 264 | 48 111 | 46 | 5 222 | 114 | 15 746 | 395 | 74 874 |
| 2019 | 451 | 81 165 | 49 | 4 679 | 43 | 5 754 | 292 | 56 710 |
| 2020 | 191 | 35 494 | 27 | 3 038 | 89 | 12 469 | 84 | 13 242 |
| 2021 | 325 | 53 645 | 48 | 5 014 | 13 | 1 453 | 38 | 4 333 |
| 2022 | 228 | 38 180 | 49 | 5 336 | 9 | 961 | 52 | 11 348 |
| 2023 | 150 | 23 230 | 44 | 3 854 | 81 | 9 659 | 34 | 4 187 |
| 2024 | 246 | 43 591 | 36 | 4 161 | 21 | 1 987 | 45 | 6 816 |
| 2025 | 289 | 50 487 | 47 | 5 532 | 25 | 3 019 | 37 | 4 818 |
Age compositions
Table 3 presents the number of otolith samples and age readings by gear type, while Figure 13 shows the sampling locations.
Over the past few decades, the age composition of the catch has shifted toward older fish, likely due to reduced fishing pressure (Figure 15). In recent years, the number of year classes represented in the catch has increased, reflecting sustained low fishing mortality (Figure 16).
| Year |
Bottom Trawl
|
Danish Seine
|
Gillnets
|
Long Line
|
||||
|---|---|---|---|---|---|---|---|---|
| Num. samples | Num. otoliths | Num. samples | Num. otoliths | Num. samples | Num. otoliths | Num. samples | Num. otoliths | |
| 2000 | 205 | 10 034 | 18 | 885 | 21 | 1 051 | 44 | 2 223 |
| 2001 | 515 | 9 193 | 10 | 500 | 288 | 2 239 | 136 | 2 830 |
| 2002 | 587 | 8 612 | 30 | 693 | 226 | 2 055 | 162 | 2 815 |
| 2003 | 684 | 8 144 | 9 | 450 | 308 | 1 217 | 170 | 3 409 |
| 2004 | 824 | 9 052 | 8 | 400 | 90 | 802 | 100 | 2 297 |
| 2005 | 654 | 6 485 | 208 | 788 | 12 | 598 | 103 | 3 548 |
| 2006 | 529 | 5 720 | 71 | 931 | 102 | 1 471 | 271 | 3 507 |
| 2007 | 625 | 6 094 | 328 | 1 244 | 125 | 1 203 | 82 | 3 650 |
| 2008 | 543 | 5 024 | 217 | 816 | 196 | 1 029 | 65 | 2 771 |
| 2009 | 569 | 5 417 | 136 | 561 | 23 | 1 150 | 33 | 1 650 |
| 2010 | 493 | 5 880 | 83 | 501 | 16 | 799 | 59 | 2 931 |
| 2011 | 340 | 5 339 | 49 | 578 | 14 | 700 | 46 | 2 294 |
| 2012 | 403 | 5 757 | 63 | 688 | 21 | 1 031 | 73 | 3 209 |
| 2013 | 375 | 6 192 | 39 | 397 | 21 | 1 050 | 62 | 3 065 |
| 2014 | 378 | 5 102 | 20 | 525 | 29 | 850 | 65 | 1 856 |
| 2015 | 312 | 4 937 | 29 | 708 | 45 | 917 | 54 | 1 467 |
| 2016 | 320 | 5 015 | 41 | 1 025 | 41 | 1 025 | 60 | 1 544 |
| 2017 | 236 | 3 817 | 39 | 975 | 26 | 644 | 46 | 1 119 |
| 2018 | 92 | 2 369 | 30 | 750 | 16 | 400 | 39 | 945 |
| 2019 | 113 | 2 828 | 27 | 675 | 12 | 300 | 50 | 1 237 |
| 2020 | 73 | 1 847 | 21 | 520 | 12 | 300 | 31 | 775 |
| 2021 | 85 | 2 171 | 34 | 850 | 8 | 200 | 30 | 750 |
| 2022 | 57 | 1 264 | 16 | 320 | 2 | 40 | 18 | 362 |
| 2023 | 79 | 1 511 | 28 | 560 | 6 | 118 | 22 | 440 |
| 2024 | 91 | 1 871 | 31 | 620 | 5 | 100 | 22 | 440 |
| 2025 | 94 | 1 916 | 30 | 600 | 5 | 100 | 17 | 340 |
Weight at age in the catch
Mean weight at age in the catch (Figure 17) declined from 2001 to 2007, reaching historical lows in many age groups. Although mean weights increased in subsequent years, nearly all age classes were at least slightly below the 1985–present average in both this year and the previous year. For 2026, mean weights for ages 3–9 are estimated using the relationship between spring survey weights and commercial weights from the preceding year. Weights for older fish are assumed to remain unchanged from the previous year (see section on short-term projections).
Survey data
The Icelandic spring groundfish survey (hereafter spring survey) has been conducted annually in March since 1985. An additional survey, the Icelandic autumn groundfish survey (autumn survey), was initiated in 1996. However, a full autumn survey was not carried out in 2011.
Figure 18 presents a recruitment index based on cod smaller than 55 cm, alongside trends in various biomass indices. Survey abundance by tow location is shown in Figure 19, while changes in spatial distribution are illustrated in Figure 20.
The total biomass index from the spring survey has remained relatively high since 2012 but has shown an overall declining trend over the past decade. Both spring and autumn survey indices declined markedly from their 2017 peak to 2020, followed by a slight increase during 2021-2024 (Figure 18). While spring survey measurements in 2021 and 2022 were similar to those in 2018 and 2019, the autumn survey index in 2021 declined further, reaching its lowest level since 2004. The 2020 survey indices were considerably below expectations for the size classes making up the majority of the fishable biomass, a trend that continued in the 2021 autumn survey but not in the 2021 spring survey.
Overall, both surveys have shown similar long-term trends (Figure 18), although fluctuations since the late 2000s have been more pronounced in the autumn survey. The discrepancy between spring and autumn biomass measurements reached a record high in 2021 and remains the largest observed since 2000. However, the recent decline in the spring survey index, combined with a stabilization in the autumn index, has narrowed this gap in the most recent survey year.
In the spring survey of 2026, cod were caught throughout Icelandic waters, with hotspots observed offshore in the northwest, southeast, and in shallow southern waters (Figure 19). Biomass along the western continental slope was similar to the previous year. The spatial distribution of the total biomass index consistently shows the north (N), northwest (NW) and northeast (NE) areas dominating across years (Figure 20). The spatial distribution of cod in the autumn survey of 2025 was similar to previous years, with the majority of biomass measured on traditional fishing grounds in the northwest (NW) and north (N) regions (Figure 20). However, recent years have seen some shifts, with the spring survey showing declining biomass in the NE and increases in the west and southeast (SE). In the same time period, the autumn survey shows an increase the northwest, both deep (dNW) and shallower areas (NW), as well as in the west (W). In 2026, biomass decreased in most areas.
Length distributions from both surveys clearly show distinct modes for the youngest age groups (Figure 21). In older age groups, separation becomes less distinct due to individual variability in growth and maturity, though modes corresponding to 2- and 3-year-old fish can sometimes be identified.
Survey age-based indices for older fish have remained relatively high over the past decade, despite the fact that many of these cohorts showed only low to moderate indices at younger ages (Figure 22). The 2020 spring survey anomaly is particularly evident — e.g., the 2014 and 2015 year classes were around the long-term average in 2019 (as 4- and 5-year-olds), but dropped to roughly half that in 2020 (as 5- and 6-year-olds). In 2021, the 2015 cohort appeared well above average in both survey and catch-at-age data, a trend that continued in subsequent years and suggests likely immigration from Greenland waters.
Stock weight at age
Mean weights in the spring survey for all cod age groups were below average during approximately 2000–2010 (Figure 23). Following this period, mean weights for ages 5–10 were generally above average for several years. However, in the past two years, mean weights have declined across both younger and older age groups.
Stock maturity at age
Maturity-at-age data from the spring survey are presented in Figure 24. In recent decades, maturity at younger ages has generally been below average, indicating a trend toward later maturation.
Stock assessment
Model and data inputs
The assessment is based on a separable statistical catch-at-age model (commonly referred to as MUPPET, see H. Björnsson, Hjörleifsson, and Elvarsson (2019)), which assumes constant selectivity within four time periods. The most recent period spans from 2007 to the present. Survey residuals are modeled using a multivariate normal distribution to account for potential year effects — an approach implemented since 2002. The model is a statistical cohort framework in which fishing mortality can change gradually over time, constrained by a random walk. This same framework is used to project stock dynamics for estimating reference points and evaluating the harvest control rule (HCR). It was benchmarked in 2021 as part of the HCR evaluation (ICES (2021b)).
In the current assessment, the model configuration was updated to account for a likely migration event. The 2015 year class appeared in 2021 at age 6 in higher numbers than would be expected based on earlier observations. To address this, an additional parameter was included beginning with the 2025 assessment to estimate recruitment at age 6 in 2021 — representing the 13th such migration event accounted for since the model’s starting year of 1955.
The assessment relies on four primary data sources: two groundfish surveys (spring and autumn), commercial samples, and landings. Commercial data are used to construct catch-at-age estimates, which enter the likelihood function alongside age-specific survey indices from both surveys. Stock weights and catch weights at age are derived from the spring survey and commercial catches, respectively, while maturity-at-age data are obtained from the spring survey. Prior to the start of the spring survey in 1985, stock weights and maturity were assumed constant at their 1985 values.
A detailed description of data preparation for both tuning and input is provided in the stock annex (ICES (2021a)), and all input data are available on the MFRI website (www.hafogvatn.is).
The input to the analytical age-based assessment consists of catch-at-age data from 1955 to 2025 (ages 3–14), spring survey data (SMB) from 1985 to 2026 (ages 1–14), and autumn survey data (SMH) from 1996 to 2025 (ages 3–13). Catch-at-age data are derived based on 20 metiers, combining two areas (north and south), two seasons (January–May and June–December), and five fleets (bottom trawl, longline, handline/jiggers, gillnet, and Danish seine).
The reference biomass (age 4+) used to set the TAC for the upcoming fishing year is calculated as the product of population numbers at the beginning of the assessment year and catch weights for that year. Since catch weights for 2026 are not yet known, they must be predicted from stock weights measured in the spring survey, using a relationship established from the previous year’s data.
Mean weight at age in the catch (Figure 17) declined between 2001 and 2007, reaching historical lows in many age groups. The observed variation in catch weights at age partly reflects underlying variability in stock weights, as indicated by survey measurements (Figure 23).
No direct information is available on natural mortality. For assessment and advisory purposes, a fixed natural mortality rate of 0.2 is assumed for all age groups.
Diagnostics and fit
The diagnostics (Figure 25) reveal large negative residuals in the 2020 spring survey for the key age groups (ages 4 to 8), along with smaller negative residuals in the surrounding the years, 2019 and 2021, particularly in the autumn survey. A summary diagnostic comparing observed and predicted survey biomass (Figure 26) highlights discrepancies between model estimates and survey point estimates. There are indications that interannual variability in survey measurements has increased in recent years in both surveys, relative to earlier periods.
Results
The results of this year’s assessment estimate the spawning stock biomass (SSB) for the assessment year at 371 thousand tonnes. The estimated SSB in recent years is higher than any values observed over the past five decades. The reference biomass for 2026 is estimated at 997633 t, and the harvest rate for 2025 is estimated at 0.198.
Year classes since the mid-1980s are estimated to be relatively stable, but with a mean approximately 35% lower than that observed during 1955–1985. Assessment results are summarized in Table 4 and Figure 27, and are also available on the MFRI website (www.hafogvatn.is).
Reference biomass has remained stable in recent years. However, the estimates for the 2021 and 2022 year classes have not been revised upward from the relatively low values reported last year (close to 100 million). These cohorts are expected to form a substantial part of the fishable stock in 2026–2027, suggesting a potential decline in fishable biomass during that period. Moreover, the most recent recruitment estimate (2023 year class) is only slightly higher and remains below the past decade’s average, indicating that the decline in reference biomass could continue into 2028, unless future recruitment estimates are revised upward.
Estimated spawning stock biomass (SSB), although variable, increased to a peak in 2017, the highest level observed in nearly 60 years. Since the most recent revision of the harvest control rule, the harvest rate has declined. Given that recruitment since 1988 has been substantially lower than the average observed during 1955–1985, the increase in SSB was primarily driven by lower harvest rate.
In 2023, the harvest rate reached its lowest level in the assessment period. However, due to the decline in stock and catch weights during the past year, a greater number of cod will be required to fill the current TAC compared to previous years. As a result, the harvest rate has increased over the last year.
This rise in fishing mortality, combined with the potential for elevated natural mortality due to lower energy reserves and increased predation on recruiting age groups (B. Björnsson, Sólmundsson, and Woods 2022), could increase the risk of overestimating stock size in projections. This potential overestimation, along with recent recruitment levels falling below the past decade’s average, suggests a continued decline in biomass is likely in the short term.
Biomass estimates have been revised upwards in each of the past three years, suggesting a slight tendency for the model to underestimate spawning stock biomass (SSB). In the current assessment, the notable upward revisions in SSB for 2021 and subsequent years result from a change in the model configuration to account for a likely migration event. Specifically, an additional parameter was introduced to estimate recruitment to the population at age 6 in 2021.
This migration event was first identified through unexpectedly high numbers of the 2015 year class appearing at age 6 in 2021, a signal that persisted through consecutive years and was consistently detected in all three data sources used in the model. The same 2015 cohort also appears as a large year class in East Greenland catch-at-age and survey data for the East Greenland–Iceland offshore spawning cod stock (ICES stock cod.21.27.1.14), indicating a likely shared origin.
This represents the 13th migration event accounted for in the model since 1958, all of which involved recruitment at ages 6–9 and were most likely associated with immigration from Greenland waters.
In addition to this 13th migration event, fishing activity and catches have increased over the past decade on both the Icelandic and Greenland sides of the EEZ near Dohrn Bank. Currently, the cod stock located on the Greenland side of the EEZ boundary is assessed using landings data only, as attempts to implement a category 1 assessment have not successfully captured trends across most fishing activities in the area. As a result, catch-at-age data are generated as part of the Greenland stock assessment. These data were included in the Icelandic stock assessment as a sensitivity run, both with and without estimation of the 13th migration event.
Omitting the 13th migration from the assessment resulted in a slight upward revision of the 2020 biomass estimate and a marginally poorer model fit. Including catch data from Dohrn Bank generally led to upward revisions of SSB estimates across the period following 2015. When both the migration event and Dohrn Bank data were included, these effects were combined; however, the inclusion of Dohrn Bank data also caused a decline in model fit. As a result, only the estimation of the 13th migration was retained in the final model configuration used for providing advice. The sharp decline in SSB projected for 2025 was consistent across all model runs.
The retrospective pattern of the assessment is shown in Figure 29, along with the Mohn’s rho values. The default 5-year peels resulted in the following values: 0.04 for recruitment, 0.007 for harvest rate, and 0.001 for spawning stock biomass.
Leave-one-out analyses indicate that the assessment aligns most closely with trends in the spring survey. Removing the autumn survey series results in a slight increase in biomass estimates, while removing the spring survey leads to a more substantial increase — similar to the effect of relying on catch data alone (Figure 30).
Short-term projections
Landings of Icelandic cod in 2025 are estimated at 218833 tonnes, the majority of which were taken by the Icelandic fleet.
To perform short-term projections, an estimate of the catch for the current calendar year is required. This year’s projection assumes that the remainder of the TAC for the current fishing year (ending August 31) will be fully taken, along with an expected 3 thousand tonnes catch by the foreign fleet. The projected stock status for the interim year, along with the projection output, is provided in Table 4.
Mean annual discards of cod during 2001–2012 were approximately 1% of landings by weight. More recent data suggest that discards may have increased slightly (MRI 2016). These discard estimates are based on the assumption that discarding primarily occurs as high-grading.
In line with the management plan, advice for the upcoming fishing year (2026/2027) is based on the biomass of age 4+ cod at the beginning of the calendar year (2026). Because reference biomass is calculated using catch weights, a deterministic projection of catch weight growth is required. In recent years, catch weights at age for age groups 3–9 have been predicted using spring survey weights from the same year, applying a linear relationship (slope and intercept) derived from the previous year’s data. For age groups 10 and older, catch weights from the previous year are carried forward.
The same method was used to estimate weights-at-age for the following year, i.e., \(\alpha\) and \(\beta\) were estimated according to the following equation:
\[ \text{cW}_{a,y-1}=\alpha+\beta\text{sW}_{a,y-1} \]
and catch weights for the assessment year were then estimated according to:
\[\text{cW}_{a,y}=\alpha+\beta\text{sW}_{a,y}\]
where cWa,y denotes the catch weight and sWa,y the stock weight for age a and year y.
Based on this approach, the predicted mean catch weights-at-age in 2026 are below average for most age groups, as both the mean weights in the spring survey and in the catch were below average in 2025, and stock weights were below average this year (Figure 23).
An alternative method, labeled ‘alt’, was also explored. This model predicts catch weight at age using age-specific spring survey weights within each year, based on data from 1990 onwards. It has previously yielded more plausible estimates of catch weights, including in the current assessment year (2026), where the deviation from the standard model was 2.5%.
Retrospective analyses indicate that this alternative model has improved predictive performance, with a lower coefficient of variation (0.035 vs. 0.050) and reduced bias (-0.0020 vs. -0.0049), as shown in Figure 31 and Figure 32.
The alternative model has been discussed by the NWWG in 2022 and subsequent years as a potential improvement over the current SPALY weight prediction model. However, it was agreed that a more extensive evaluation should be conducted before implementation, especially in light of recent changes in cod mean weights. External review, either through a working document or during the next benchmark (anticipated for 2027), would also be beneficial.
Figure 33 shows the contribution of each year-class to the reference stock (B4+). The effects of reduced mean weights are clearly visible there, as for example the biomass of the 2019 year-class is at the average despite having been among the largest since 1985. The year-classes following it are weaker, however, and therefore their biomass is below average.
| Year | Calendar Year Catch | Fishing Year Catch | SSB | TB | B4+ | HR | Recruit. (age 3) |
|---|---|---|---|---|---|---|---|
| 1955 | 545 250 | — | 764 535 | 1 632 037 | 2 091 845 | 0.242 | 151 049 |
| 1956 | 486 909 | — | 615 238 | 1 475 627 | 1 819 507 | 0.256 | 143 790 |
| 1957 | 455 182 | — | 592 727 | 1 384 486 | 1 640 699 | 0.303 | 161 494 |
| 1958 | 517 359 | — | 705 112 | 1 448 341 | 1 651 300 | 0.290 | 215 083 |
| 1959 | 459 081 | — | 655 394 | 1 323 477 | 1 581 171 | 0.295 | 303 446 |
| 1960 | 470 121 | — | 603 851 | 1 332 908 | 1 657 104 | 0.246 | 153 937 |
| 1961 | 377 291 | — | 477 947 | 1 076 590 | 1 430 191 | 0.269 | 195 919 |
| 1962 | 388 985 | — | 515 106 | 1 171 146 | 1 464 140 | 0.275 | 125 540 |
| 1963 | 408 800 | — | 471 699 | 1 119 835 | 1 299 173 | 0.329 | 173 369 |
| 1964 | 437 012 | — | 431 795 | 1 060 074 | 1 211 498 | 0.333 | 197 658 |
| 1965 | 387 106 | — | 331 197 | 885 864 | 1 053 336 | 0.346 | 219 503 |
| 1966 | 353 357 | — | 301 796 | 938 337 | 1 063 586 | 0.321 | 232 913 |
| 1967 | 335 721 | — | 283 895 | 989 547 | 1 139 607 | 0.322 | 319 526 |
| 1968 | 381 770 | — | 251 038 | 990 942 | 1 241 848 | 0.319 | 171 449 |
| 1969 | 403 205 | — | 357 150 | 1 111 978 | 1 335 715 | 0.338 | 239 617 |
| 1970 | 475 077 | — | 359 976 | 1 045 550 | 1 332 679 | 0.341 | 179 805 |
| 1971 | 444 248 | — | 259 647 | 874 821 | 1 083 791 | 0.380 | 193 106 |
| 1972 | 395 166 | — | 235 411 | 776 253 | 979 028 | 0.386 | 142 291 |
| 1973 | 369 205 | — | 250 229 | 724 243 | 831 340 | 0.443 | 277 764 |
| 1974 | 368 133 | — | 192 139 | 745 624 | 909 778 | 0.402 | 187 287 |
| 1975 | 364 754 | — | 175 446 | 796 852 | 891 575 | 0.395 | 259 142 |
| 1976 | 346 253 | — | 146 633 | 925 203 | 948 692 | 0.361 | 367 732 |
| 1977 | 340 086 | — | 199 221 | 1 024 910 | 1 296 121 | 0.257 | 144 417 |
| 1978 | 329 602 | — | 213 709 | 1 130 779 | 1 307 062 | 0.271 | 224 301 |
| 1979 | 366 462 | — | 308 504 | 1 233 571 | 1 408 725 | 0.291 | 237 488 |
| 1980 | 432 237 | — | 375 669 | 1 239 277 | 1 511 307 | 0.300 | 141 616 |
| 1981 | 465 032 | — | 286 039 | 1 011 190 | 1 254 580 | 0.326 | 145 485 |
| 1982 | 380 068 | — | 189 146 | 796 336 | 987 942 | 0.329 | 141 313 |
| 1983 | 298 049 | — | 147 038 | 690 136 | 803 657 | 0.358 | 227 772 |
| 1984 | 282 022 | — | 156 291 | 763 100 | 915 285 | 0.338 | 143 957 |
| 1985 | 323 428 | — | 169 099 | 724 261 | 942 925 | 0.372 | 140 464 |
| 1986 | 364 797 | — | 194 155 | 900 518 | 869 564 | 0.439 | 297 879 |
| 1987 | 389 915 | — | 145 942 | 818 409 | 989 057 | 0.386 | 249 599 |
| 1988 | 377 554 | — | 154 704 | 783 269 | 976 472 | 0.377 | 176 465 |
| 1989 | 363 125 | — | 158 427 | 767 882 | 948 210 | 0.363 | 97 241 |
| 1990 | 335 316 | — | 195 078 | 707 759 | 815 738 | 0.389 | 130 198 |
| 1991 | 307 759 | — | 158 063 | 622 122 | 698 530 | 0.400 | 113 208 |
| 1992 | 264 834 | — | 143 908 | 512 822 | 565 899 | 0.451 | 159 452 |
| 1993 | 250 704 | — | 111 801 | 494 202 | 584 908 | 0.346 | 129 531 |
| 1994 | 178 138 | — | 146 713 | 515 480 | 567 871 | 0.302 | 80 796 |
| 1995 | 168 592 | — | 167 999 | 542 478 | 565 029 | 0.313 | 141 783 |
| 1996 | 180 701 | — | 154 790 | 600 967 | 678 451 | 0.288 | 165 858 |
| 1997 | 203 112 | — | 189 133 | 656 613 | 795 756 | 0.289 | 92 062 |
| 1998 | 243 987 | — | 198 850 | 656 326 | 737 973 | 0.345 | 155 615 |
| 1999 | 260 147 | — | 175 865 | 597 872 | 727 691 | 0.335 | 75 982 |
| 2000 | 235 092 | — | 162 629 | 563 778 | 589 922 | 0.400 | 167 229 |
| 2001 | 236 702 | — | 158 097 | 566 140 | 663 217 | 0.330 | 155 076 |
| 2002 | 209 544 | — | 188 177 | 615 779 | 712 875 | 0.292 | 157 738 |
| 2003 | 207 246 | — | 185 822 | 652 106 | 741 151 | 0.299 | 180 494 |
| 2004 | 228 342 | — | 192 502 | 661 275 | 810 918 | 0.270 | 84 982 |
| 2005 | 213 867 | — | 222 850 | 623 287 | 728 518 | 0.278 | 154 854 |
| 2006 | 197 202 | — | 216 942 | 603 090 | 692 337 | 0.260 | 132 236 |
| 2007 | 171 646 | — | 203 591 | 575 549 | 668 735 | 0.233 | 95 020 |
| 2008 | 147 676 | — | 254 796 | 587 056 | 673 016 | 0.255 | 130 966 |
| 2009 | 183 320 | — | 235 989 | 617 433 | 747 266 | 0.233 | 117 018 |
| 2010 | 170 025 | — | 267 129 | 665 566 | 795 951 | 0.215 | 125 591 |
| 2011 | 172 218 | — | 326 630 | 795 791 | 842 886 | 0.223 | 165 032 |
| 2012 | 196 171 | — | 362 058 | 895 484 | 962 694 | 0.223 | 175 230 |
| 2013 | 223 582 | — | 386 545 | 950 914 | 1 084 928 | 0.205 | 124 827 |
| 2014 | 222 021 | — | 353 606 | 913 287 | 1 091 620 | 0.208 | 173 857 |
| 2015 | 230 165 | — | 459 866 | 1 026 359 | 1 172 212 | 0.208 | 147 841 |
| 2016 | 251 219 | — | 403 571 | 994 077 | 1 226 339 | 0.201 | 99 566 |
| 2017 | 243 945 | — | 532 327 | 1 078 921 | 1 154 596 | 0.225 | 153 500 |
| 2018 | 267 221 | — | 522 334 | 1 044 172 | 1 198 198 | 0.221 | 154 015 |
| 2019 | 263 025 | — | 466 865 | 984 204 | 1 126 977 | 0.238 | 119 060 |
| 2020 | 270 302 | — | 411 336 | 958 569 | 1 018 844 | 0.262 | 145 557 |
| 2021 | 265 740 | — | 410 383 | 966 420 | 1 125 663 | 0.222 | 133 637 |
| 2022 | 242 208 | — | 423 614 | 942 477 | 1 107 037 | 0.204 | 173 334 |
| 2023 | 217 847 | — | 404 546 | 885 533 | 1 156 803 | 0.190 | 134 292 |
| 2024 | 220 340 | — | 378 080 | 816 798 | 1 067 887 | 0.205 | 101 582 |
| 2025 | 218 683 | — | 367 679 | 783 179 | 1 050 402 | 0.198 | 115 029 |
| 2026 | 202 367 | 201.674 | 377 277 | 736 796 | 997 633 | — | 132 259 |
| 2027 | 201 397 | 201.016 | 377 344 | — | 1 001 786 | — | 133 469 |
| 2028 | — | 201.107 | 369 437 | — | 1 005 989 | — | 115 513 |
Management
History
The Ministry of Industries is responsible for the management of Icelandic fisheries and implementation of relevant legislation. Cod was incorporated into the Individual Transferable Quota (ITQ) system in 1984. During the early years of the Total Allowable Catch (TAC) system, effort management was also implemented, partly to address concerns from stakeholders who felt they had received an unfair share of the quota. This “additional effort” management system resulted in catches exceeding the TAC by 20–30% in the initial years of the ITQ system.
In 1990, legislation was amended to eliminate effort management, except for the smallest coastal fleet, which remained under a fishing days regime. At the same time, many restrictions on quota transferability were lifted, and the fishing year was redefined to run from 1 September to 31 August. These changes took effect on 1 September 1991. In the early 1990s, scientific advice from the Marine Research Institute (MRI) was based on reducing fishing mortality (F) by 40%. However, during this period, TACs exceeded scientific advice, and catches exceeded TACs.
The cod stock declined sharply in the early 1990s due to a combination of low recruitment and high fishing mortality. Recognizing the need for stricter fisheries control, a group of fisheries scientists developed a Harvest Control Rule (HCR), which was adopted for the 1995/96 fishing year. This led to a significant reduction in fishing mortality.
Since the introduction of the HCR, TACs have been set according to the rule. However, catches have exceeded TACs by an average of approximately 5% in recent years (Figure 34). The primary reason for this overage is that catches from vessels operating under the effort control system have exceeded predictions. These predicted catches are deducted from the TAC calculated under the HCR before allocating the remaining quota to Icelandic vessels.
The TAC system does not account for catches taken by Norway and the Faroe Islands under bilateral agreements. Although the size of these catches is known in advance, they were not historically considered in the Ministry’s TAC allocation to Icelandic vessels.
There is no minimum landing size for cod in ICES Division 5.a. However, economic penalties are imposed on landings valued below a minimum size threshold to discourage such practices. Iceland, Norway, and the Faroe Islands also maintain bilateral agreements governing fishing access to restricted areas within Iceland’s EEZ. Under these agreements, Faroese vessels are permitted to catch up to 5,600 tonnes of demersal fish species in Icelandic waters, including a maximum of 1,200 tonnes of cod.
Catches from Marine and Freshwater Research Institute surveys are outside vessel quotas; this catch has typically accounted for approximately 0.5 to 1.5% of the total cod catch. Other catches not included in vessel quotas (so-called VS-catch) have increased in recent years, rising from less than 0.5% to over 1.5% in 2024/2025 (Figure 36).
Harvest control rule
The TAC for the next fishing year (starting 1 September in the assessment year and ending 31 August of the following year) is based on a multiplier of 0.20 applied to the reference biomass of fish aged four years and older in the assessment year (\(B_{4+,y}\)). A stabiliser is then applied by averaging this result with the previous year’s TAC to determine the TAC for the next fishing year:
\[ \mathrm{TAC}_{y+1} = \frac{0.20 \cdot B_{4+,y} + \mathrm{TAC}_y}{2} \]
If the spawning stock biomass (SSB) is below the trigger value of 220,000 tonnes, the stabiliser is not applied. Instead, the harvest rate is scaled linearly according to the ratio of SSB to the trigger value:
\[ \mathrm{TAC}_{y/y+1} = 0.20 \cdot B_{4+,y} \cdot \frac{\mathrm{SSB}_y}{220{,}000} \]
Information regarding management strategies and harvest control rules can be found on the Government of Iceland webpage here.
A system of catch-quota balancing allowances is in place that permits quota transfers between years and some species transformations, as illustrated in Figure 35. Transfers into cod from other species are not allowed. Net quota transfers out of cod to other species have remained relatively low in recent years (Figure 35, upper panel). Transfers of unused cod quota between fishing years typically range from 0–7%.
The harvest control rule (HCR) has undergone several amendments over time. The most recent significant change occurred in 2007, when the harvest rate multiplier used to determine TAC was reduced from 0.25 to 0.20. The current HCR also includes a catch stabiliser: when SSB in the assessment year is estimated to exceed 220 thousand tonnes, the rule applies the averaging procedure as shown above.
The TAC set for the current fishing year (2025/2026), based on last year’s assessment, was 203822.
Following the 2021 benchmark, the reference biomass used in advice was estimated to be approximately 20% lower in recent years than under the previous framework. This has contributed to slightly higher realized harvest rates than intended, although these remain within the expected range of the HCR simulations. During the benchmark, reference points and the definition of harvest rate were also revised.
Management considerations
Both spring and autumn survey indices are on par with values closer to 2010. The most recent catch weights (2025) have increased slightly. However, stock weights remain low for most year classes, and both catch and stock weights have been below the long-term average for the past three years, especially for year classes composing the fishable stock. Unexpectedly low weights at age in the catch will result in higher fishing mortality. In addition, reduced energy reserves and lower prey availability could lead to increased natural mortality. Together, these factors increase the risk of stock size declining in the near future.
Despite this, commercial catch data and surveys indicate that cod in Division 5.a is currently in good condition. This is supported by the stock assessment and the most recent HCR evaluation (ICES 2021b). While the stock is presently in a strong state, the highly variable recruitment observed over the past decade suggests future fluctuations in stock size are likely. The assessment model has a tendency to underestimate catches in the most recent 5 years, and may therefore also slightly underestimate harvest rates, but this discrepancy is expected to be minor (for example, realized harvest rate in 2025 may be closer to 0.21 rather than 0.198).
Current recruitment estimates for the 2020–2022 year classes remain below the decade average. The 2023 year class is estimated closer to average, but the earliest view of the the two youngest year classes (age 1 & 2 indices in the surveys, year classes 2024–2025) do not show any marked increase in survey index values compared to the previous 5 years. As these low recruitment years occur consecutively, a decline in reference biomass can be expected in the coming years unless stronger recruitment is observed. However, because the HCR includes a cap on changes in TAC, the impact of this decline will be moderated in future advice.
Ecosystem considerations
Stock and catch weights-at-ages have been lower than the long-term average for most ages over the past three years, especially in age classes that currently dominate the reference biomass. As capelin is known to be a major prey source for cod in Icelandic waters (Pálsson and Björnsson (2011)) and capelin stock levels have been linked to cod growth (Frater et al. (2019)), the reduction in cod weights is likely linked to low levels of capelin (ICES stock cap.27.2a514) in Icelandic and Faroese waters, East Greenland, and the Jan Mayen area in recent years.
In addition, recent and historical patterns of common cohort strength shared between this stock and the East Greenland–Iceland offshore spawning cod stock (cod.21.27.1.14) suggest linkages in productivity and periodic migrations. These linkages have not been quantified but may affect assumptions of stock boundaries, stock productivity, and sustainable fishing rates.