| Year | Nr. Bottom Trawl | Nr. Gillnets | Nr. Long Line | Bottom Trawl | Gillnets | Long Line | Other | Total catch |
|---|---|---|---|---|---|---|---|---|
| 2000 | 125 | 184 | 289 | 726 | 704 | 1 540 | 70 | 3 284 |
| 2001 | 108 | 232 | 254 | 493 | 1 061 | 1 101 | 481 | 3 362 |
| 2002 | 100 | 203 | 235 | 664 | 648 | 1 283 | 1 674 | 4 519 |
| 2003 | 96 | 172 | 244 | 583 | 454 | 2 215 | 680 | 4 270 |
| 2004 | 97 | 165 | 234 | 656 | 545 | 2 017 | 886 | 4 606 |
| 2005 | 99 | 127 | 260 | 989 | 501 | 2 046 | 896 | 5 198 |
| 2006 | 91 | 99 | 259 | 1 246 | 629 | 3 734 | 1 124 | 7 404 |
| 2007 | 91 | 86 | 251 | 1 395 | 633 | 4 042 | 1 030 | 7 591 |
| 2008 | 82 | 68 | 209 | 1 509 | 477 | 5 007 | 1 576 | 9 283 |
| 2009 | 77 | 78 | 208 | 1 540 | 723 | 6 232 | 1 184 | 10 773 |
| 2010 | 75 | 69 | 197 | 1 538 | 363 | 6 532 | 1 124 | 10 963 |
| 2011 | 67 | 61 | 201 | 1 676 | 222 | 5 595 | 857 | 9 626 |
| 2012 | 68 | 62 | 206 | 1 396 | 245 | 7 479 | 1 143 | 11 817 |
| 2013 | 71 | 62 | 209 | 1 610 | 345 | 6 836 | 1 334 | 11 581 |
| 2014 | 64 | 57 | 220 | 1 707 | 673 | 10 624 | 12 | 14 246 |
| 2015 | 64 | 55 | 207 | 1 911 | 650 | 9 249 | 6 | 13 035 |
| 2016 | 65 | 55 | 186 | 1 825 | 681 | 6 545 | 9 | 9 884 |
| 2017 | 67 | 48 | 171 | 1 527 | 556 | 5 975 | 5 | 8 766 |
| 2018 | 63 | 47 | 151 | 1 606 | 387 | 5 366 | 11 | 8 062 |
| 2019 | 61 | 33 | 148 | 1 666 | 115 | 5 964 | 2 | 8 269 |
| 2020 | 63 | 36 | 124 | 1 677 | 138 | 4 765 | 6 | 7 061 |
| 2021 | 64 | 39 | 119 | 1 836 | 126 | 4 829 | 3 | 7 128 |
| 2022 | 62 | 30 | 103 | 2 232 | 262 | 4 917 | 0 | 7 657 |
| 2023 | 58 | 32 | 88 | 2 518 | 176 | 5 652 | 0 | 8 560 |
| 2024 | 59 | 30 | 80 | 2 573 | 159 | 5 898 | 0 | 8 868 |
| 2025 | 53 | 30 | 84 | 2 722 | 216 | 6 534 | 0 | 9 791 |
Key signals
Total stock biomass observed in the spring survey declined steadily from 1985 to 2000, when it increased again and reached a high level in 2011-2012. Subsequently in decreased again, but since 2021 biomass has increased and is currently at one of the highest levels observed.
Abundance of small ling (<40 cm) in the spring survey peaked in 2007 and was high until 2010, when it decreased substantially to very low levels in 2012. Since 2020, the abundance has been increasing steadily. Length distributions from the spring survey show a similar pattern as survey indices, with the 2012-2018 peak in abundance observed as high proportions of fish in the range of 60–100 cm, that has slowly decreased as they have reached sizes 80–120 cm.
Biomass of large ling (>80 cm) in the spring survey was relatively stable from 1985 to 2001, but has since increased and is now at the highest level recorded.
Fishing mortality (F, ages 8–11) has generally declined since 1984 and in 2022 and 2023 was below FMGT. In 2024 and 2025 it increased slightly and was above FMGT, but remains below FPA and Flim.
Recruitment increased rapidly from 1999 until 2008, when it reached its highest level. Since then, recruitment decreased and is now at similar levels as before the increase.
General information
The common ling is one of the largest fish of the Gadiformes order reaching a maximum length of 200 cm, with a mean length of about 70-90 cm according to data from the annual Icelandic spring groundfish survey. It is a demersal fish that preys on fish and invertebrates and can be found at depths 10 and 1300 meters but is mainly caught at depths between 100 and 400 meters. It reaches sexual maturity at the age of 5-8 years and 60-80 cm total length. Ling spawns in May and June mostly along the edges of the south, southwest and west of the Icelandic continental shelf.
Fishery
Landings trends
In 1947 to 1971, landings of ling from Icelandic waters ranged between 8000 to more than 15000 tonnes. Landings decreased between 1972 and 2000 to as little as 3000 tonnes as a result of most foreign vessels being excluded from the Icelandic EEZ. In 2001-2010, catches increased constantly and reached 11 000 tonnes in 2010 and remained at that level for the most part until 2014, when the catches increased to 14 000 tonnes. Since 2014, ling catches have reduced, but increased again after 2021, and in 2025, 9791 tonnes were landed (Table 1 and Figure 1)
The fishery for ling in Icelandic waters has not changed substantially in recent years. Around 100-300 longliners annually report catches of ling, around 30-200 gillnetters and around 50-120 trawlers. Most of ling is caught on longlines (Figure 2, Table 1) which has increased since 2000 to around 67 % in 2025. At the same time the proportion caught by gillnets has decreased from 20–30% in 2000–2007 to approximately 2% in 2025. Catches in trawls have varied less and have been at around 20-30% of Icelandic catches (Figure 2). Most of the ling caught by Icelandic longliners is caught at depths less than 300 m, and by trawlers at less than 400 m (Figure 3). The main fishing grounds for ling as observed from logbooks are in the south, southwestern and western part of the Icelandic shelf (Figure 4). The main trend in the spatial distribution of catches according to logbook entries is the decreased proportion of catches in the southeast and increased catches on the western part of the shelf two decades ago. Around 50% of ling catches are caught on the southwestern part of the shelf (Figure 5). In recent years, the main fishing pressure has shifted towards shallower waters (Figure 3).
Landings and discards
Data on landings by Icelandic vessels are collected by the Icelandic Directorate of Fisheries. Landings of Norwegian and Faroese vessels are registered through the Icelandic Coast Guard. Discarding is banned by law in the Icelandic demersal fishery. Based on limited data, discard rates in the Icelandic longline fishery for ling are estimated very low (<1% in either numbers or weight) (WGDEEP, ICES 2011:WD02). Measures in the management system such as converting quota share from one species to another are used by the fleet to a large extent and this is thought to discourage discarding in mixed fisheries.
Data and sampling
In general sampling is considered good from commercial catches from the main gears and seems to cover the spatial distribution of catches (Figure 6). Similarly, sampling does seem to follow the temporal distribution of catches (Figure 6).
Length compositions
Most length measurements of ling are from longlines and bottom trawls (Table 2). The number of available length measurements increased in recent years in line with increased landings but in 2020 they were fewer (due to the covid pandemic). Length distributions from the Icelandic longline and trawling fleet are presented in Figure 7. Sampling from commercial catches of ling is considered good; both in terms of spatial and temporal distribution of samples (Figure 6).
| Year | Trawls | Demersal seine | Gillnets | Longlines | Other | Total |
|---|---|---|---|---|---|---|
| 2000 | 377 | 0 | 566 | 1 624 | 6 | 2 573 |
| 2001 | 37 | 0 | 493 | 1 661 | 0 | 2 191 |
| 2002 | 221 | 0 | 366 | 1 504 | 0 | 2 091 |
| 2003 | 137 | 0 | 300 | 2 405 | 143 | 2 985 |
| 2004 | 141 | 46 | 348 | 2 640 | 0 | 3 175 |
| 2005 | 349 | 101 | 31 | 2 323 | 150 | 2 954 |
| 2006 | 1 157 | 0 | 645 | 3 354 | 401 | 5 557 |
| 2007 | 400 | 76 | 0 | 3 661 | 0 | 4 137 |
| 2008 | 819 | 15 | 357 | 5 847 | 150 | 7 188 |
| 2009 | 516 | 0 | 410 | 9 014 | 450 | 10 390 |
| 2010 | 1 146 | 0 | 57 | 7 322 | 1 199 | 9 724 |
| 2011 | 1 245 | 150 | 0 | 7 248 | 750 | 9 393 |
| 2012 | 1 411 | 150 | 85 | 11 356 | 1 337 | 14 339 |
| 2013 | 993 | 122 | 267 | 9 405 | 1 344 | 12 131 |
| 2014 | 2 089 | 120 | 1 286 | 6 448 | 2 964 | 12 907 |
| 2015 | 2 615 | 0 | 1 563 | 3 315 | 3 052 | 10 545 |
| 2016 | 2 460 | 0 | 2 039 | 2 483 | 1 212 | 8 194 |
| 2017 | 1 963 | 0 | 485 | 1 637 | 1 226 | 5 311 |
| 2018 | 1 603 | 0 | 559 | 1 424 | 712 | 4 298 |
| 2019 | 1 830 | 0 | 0 | 3 598 | 819 | 6 247 |
| 2020 | 1 718 | 0 | 124 | 1 099 | 498 | 3 439 |
| 2021 | 2 028 | 0 | 0 | 1 056 | 466 | 3 550 |
| 2022 | 1 805 | 0 | 370 | 563 | 1 534 | 4 272 |
| 2023 | 2 423 | 0 | 90 | 1 284 | 0 | 3 797 |
| 2024 | 1 434 | 134 | 0 | 1 660 | 0 | 3 228 |
| 2025 | 3 035 | 0 | 258 | 2 452 | 0 | 5 745 |
Age compositions
Aged data are available from 2000 onwards (Table 3). In previous years, most of the ling caught in the Icelandic spring survey were between age 5 and 8 but from longlines the age was between 6 and 9. The past several years have shown a much larger composition of older fish, common up to 12, from both sample sources (see Survey Data, next section).
| Year | Longlines | Gillnets | Demersal seine | Trawls | Other | Total |
|---|---|---|---|---|---|---|
| 2000 | 650 | 200 | 0 | 150 | 0 | 1 000 |
| 2001 | 550 | 193 | 0 | 37 | 0 | 780 |
| 2002 | 519 | 166 | 0 | 150 | 0 | 835 |
| 2003 | 900 | 100 | 0 | 100 | 50 | 1 150 |
| 2004 | 750 | 100 | 46 | 100 | 0 | 996 |
| 2005 | 750 | 0 | 0 | 181 | 50 | 981 |
| 2006 | 1 137 | 288 | 0 | 450 | 100 | 1 975 |
| 2007 | 1 300 | 0 | 50 | 100 | 0 | 1 450 |
| 2008 | 1 950 | 150 | 0 | 315 | 50 | 2 465 |
| 2009 | 2 550 | 150 | 0 | 250 | 150 | 3 100 |
| 2010 | 2 498 | 50 | 0 | 450 | 400 | 3 398 |
| 2011 | 2 546 | 0 | 50 | 450 | 250 | 3 296 |
| 2012 | 3 521 | 50 | 50 | 541 | 400 | 4 562 |
| 2013 | 2 590 | 100 | 50 | 350 | 450 | 3 540 |
| 2014 | 665 | 225 | 20 | 399 | 514 | 1 823 |
| 2015 | 595 | 300 | 0 | 483 | 520 | 1 898 |
| 2016 | 440 | 345 | 0 | 460 | 220 | 1 465 |
| 2017 | 310 | 85 | 0 | 370 | 225 | 990 |
| 2018 | 245 | 100 | 0 | 310 | 120 | 775 |
| 2019 | 385 | 0 | 0 | 340 | 140 | 865 |
| 2020 | 225 | 40 | 0 | 355 | 102 | 722 |
| 2021 | 180 | 0 | 0 | 398 | 100 | 678 |
| 2022 | 183 | 80 | 0 | 400 | 318 | 981 |
| 2023 | 320 | 20 | 0 | 564 | 0 | 904 |
| 2024 | 340 | 0 | 40 | 359 | 0 | 739 |
| 2025 | 420 | 60 | 0 | 565 | 0 | 1 045 |
Weight at age in catch
Mean weight at age in the catch is shown in Figure 10. Catch weights of the older year classes (8-12 years) have been increasing in recent years and have mostly been above average since 2018. The opposite is seen in catch weights of younger age classes, where the mean weight has been below the average for the past years.
Survey data
The CPUE estimates of ling from commercial fisheries in Icelandic waters have not been considered representative of stock abundance.
Survey data
The Icelandic spring groundfish survey, which has been conducted annually in March since 1985, covers the most important distribution area of the ling fishery. In addition, the autumn survey was commenced in 1996 and expanded in 2000, however a full autumn survey was not conducted in 2011 and therefore the results for 2011 are not presented.
Figure 11 shows distribution of ling in groundfish surveys in spring 2026 and autumn 2025. Figure 12 shows both a recruitment index and the trends in biomass from both surveys. Length distributions from the spring survey are shown in Figure 13 (abundance) and changes in spatial distribution in the spring survey are presented in (Figure 14).
Ling in both the spring and autumn surveys are mainly found in the deeper waters south and west off Iceland. Both the total biomass index and the index of the fishable biomass (>40 cm) gradually decreased in the spring survey until 1995 (Figure 12). In the years 1995-2003 these indices were half of the mean from 1985–1989. In 2003-2007, the recruitment indices increased and remained high until 2010. The index of the large ling (80 cm and larger) shows a similar trend as the total biomass index (Figure 12). The recruitment index of ling, defined here as ling smaller than 40 cm, showed a considerable increase in 2003-2007 and remained high until 2010. Then the juvenile index fell to a very low level in 2014 and remained low until 2021. Since then, the recruitment indices have been ascending, as well as the indices of larger fish as it reached the highest recorded value in the time series in 2024 (Figure 12).
Length distributions from the spring survey show a similar pattern as survey indices, with the 2012-2018 peak in abundance observed as high proportions of fish in the range of 60–100 cm, that has slowly decreased as they have reached sizes 80–120 cm (Figure 13). This pattern is likely to have caused the increase in ling sizes observed in the trawl samples (Figure 7).
Biomass indices in the autumn survey were low in 1996-2000 but have increased since then (Figure 12). There is consistency between the two surveys; the autumn survey biomass indices are however derived from substantially fewer ling caught. Also, there is an inconsistency in recruitment indices (<40 cm), where the autumn survey shows much lower recruitment, in absolute terms compared with the spring survey (Figure 12). This discrepancy is likely a result of much lower catchability of small ling (due to different gears) in the autumn survey, where ling less than 40 cm has rarely been caught.
Changes in spatial distribution as observed in surveys: According to the spring survey most of the increase during the 2012–2018 peak in ling abundance was in the western area, but an increase was seen in most areas. However, most of the index in terms of biomass comes from the southwestern area or around 40% compared to around 30% between 2003 and 2011. Since 2016, the amounts of biomass in the west and southwest have, however, reduced while the proportions in the southeast have increased, leading to a greater contribution of ling from the northwest and southeast to the total index. A similar pattern is observed in the autumn survey.