Population trend
Trend
Humpback Whale stocks were heavily depleted throughout most of the southern hemisphere in the early 20th century by a combination of coastal catches in their wintering grounds, catches from land stations, and by pelagic fleets in their Antarctic feeding grounds. Approximately 220,000 Humpback Whales were taken in total, of which about 100,000 since 1940. Almost half of these latter whales consisted of illegal takes by the USSR (Zemsky et al. 1996, Allison 2006). Between 1908 and 1963, recorded catches outside the Antarctic (north of 40°S) have been: about 30,000 off the western coast of Africa (primarily Gabon and Angola); and nearly 20,000 off the eastern coasts of southern Africa (KwaZulu-Natal, Mozambique and Madagascar) and in the western Indian Ocean. For Humpback Whales in the South Atlantic, western and northern Indian Oceans, there is strong population structure between Breeding Stocks A, B, C and X (Rosenbaum et al. 2009) and evidence of some substructure within the stocks, with subunits that are spatially and genetically isolated to varying degrees. There have been records of whales âswitchingâ between the Indian and Atlantic Ocean wintering grounds but this is regarded as highly unusual (Pomilla and Rosenbaum 2005, Stevick et al. 2011).
Recent estimates of abundance for the majority of breeding stocks have been acquired using line-transect surveys as well as photographic identification capture-recapture methods. The rate of increase in abundance has been identified from time-series data. For five of these stocks, a rate of increase between 4.5% and 10.5% per year has been revealed (Leaper et al. 2008). The southern hemisphere estimate of 140,000 individuals (Jackson et al. 2015) is probably an underestimate, because there is currently no data for Stock F (South Pacific), or part of Stock Bâs winter range for a discrete period. Additionally, the entire population does not always migrate to the wintering grounds identified, for example, results revealed an excess of males during a winter census (Reilly et al. 2008).
South of 60°S, in the Antarctic, summer estimates of abundance have been conducted by the International Decade of Cetacean Research, IDCR (presently Southern Ocean Whale and Ecosystem Research, SOWER). Since 1978 and 1979, three sets of circumpolar surveys have been completed, revealing abundance estimates of 7,100 (1978â1984), 10,200 (1985â1991), and 41,800 (1992â2004). These are likely to be underestimates of the southern hemisphere population, due to the fact that not all individuals migrate south of 60°S, and a large proportion of key summer feeding grounds north of this limit have not been assessed (for example South Georgia, the South Sandwich Islands and the waters around Bouvet Island).
In the Indian Ocean, 8,000 Humpback Whales were reportedly caught from Stock C off South Africa and Mozambique between 1908 and 1915. Smaller catches took place off the KwaZulu-Natal coastline from 1920 to 1962, but significantly larger catches off Madagascar took place during two periods between 1937â1939 and 1949â1950 (Angot 1951). A certain degree of whaling in and around the Antarctic region also may have affected Breeding Stock C during the peak whaling period. Breeding Stock C has certainly recovered since the end of commercial whaling. IWC models suggest recovery of 65â96% pre-exploitation levels for the C1 stock, and Findlay et al. (2011), using shore-based surveys at Cape Vidal, calculated a significant population increase between 9% and 11.5% from 1988 to 2002. This is very similar to increase rates calculated at the same site between 1988 and 1991: 11.4â12.2%, with the best population estimate in 1990 being 1,711 individuals (Findlay and Best 1996). The population in the SW Indian Ocean is probably nearing carrying capacity and the rate of increase is expected to decline (Findlay et al. 2011). Johnston and Butterworth (2009), using a Bayesian mixed model stock assessment for sub-stocks C1 and C2+3, calculated a post-2006 abundance of > 7,000 each, meaning that C1 is estimated at 85% of pristine level and C2+3 at 55% pristine.
Subpopulation B declined considerably in the 19th and 20th centuries as a direct result of whaling in its wintering breeding grounds off the west coast of Africa. Between 1909 and 1960, approximately 30,000 Humpback Whales were documented as caught off the west coast of sub-Saharan Africa (Reilly et al. 2008). The most recent large Humpback whaling operation by Norwegian and French whalers in the waters off Gabon and São Tomé took more than 4,000 Humpbacks between 1951 and 1954, and subsequently 160 were caught off Gabon in 1959 in a final commercial whaling operation. The population dynamics of Breeding Stock B are largely uncertain, and although numbers may have increased somewhat, it is a unique assemblage, and fairly localised around a critical habitat (Benguela upwelling). Based on genetic dissimilarities, some suggest that two sub-stocks exist: specifically, B1 that spends winter off the west coast of Gabon, the Congo, Cabinda (Angola) and northwards to the Bight of Benin; and B2 with a wintering area that is currently uncertain, although may be south of that of B1 (Best 2011). Individuals off Namibiaâs west coast have not shown matches with any other site (Elwen et al. 2014), thus supporting the existence of the B2 stock. There are also records of Humpbacks during summer near Cape Verde (Hazevoet et al. 2011), but it is not clear how these relate to the greater B Stock. Movements of 11 individuals that were tracked during migrations from West Africa to Gabon indicate that these stocks are not reproductively isolated (Barendse et al. 2011, Carvalho et al. 2014).
The complex population structure of Breeding Stock B and lack of data collected from the area between Walvis Bay and northern Angola has hampered accurate overall population estimates. The most recent estimate based on capture-recapture models for data collected from 2001â2007 of whales making use of the feeding ground along the west coast is about 500 animals (Barendse et al. 2011). Without a historical baseline it is difficult to infer a recovery rate. However, the early depletion of Humpbacks off the southwestern Cape by 1914 (1,299 were taken between 1909 and 1916) and no recovery in numbers (Best and Allison 2010) up to full protection in 1963 suggests that this does represent a unique sub-group of whales that show maternally derived site fidelity to the Saldanha Bay/St Helena Bay coastal migratory corridor/feeding ground areas (Barendse et al. 2013). Other Humpbacks from Gabon make use of more offshore migratory routes (Rosenbaum et al. 2014). Modelling done for IWC, based on historic catches and capture-recapture, suggests that for âB2â the estimated abundance relative to pristine levels may be between 4.5â12.4%, but there is much uncertainty about which model configuration is appropriate (Müller et al. 2011). This uncertainty has not changed much with the most recent synthesis (Jackson et al. 2015).
The Humpback Whale is better studied than other Balaenopterid species and migratory destinations are well known for some subpopulations. The IWC Scientific Committee suggests that globally Humpback Whale stocks have generally recovered to levels at or above those of their 1940 abundance. However, the IWC is yet to assess populations in the North Pacific and four of the seven southern hemisphere stocks, thus it is currently not possible to accurately compare the global population level to that of the historic 1940 level. However, there is little evidence to suggest that the global population remains below 50% of the 1940 threshold.