Eye in the sky: tracking harmful algal blooms with satellite remote sensing

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Hoe Chang, Ken Richardson, Michael Uddstrom, and Matt Pinkerton combined ground observations and satellite remote sensing to track algal blooms on the northeast coast of New Zealand in 2002.
The dramatic appearance of a ‘red tide’ algal bloom at Leigh, near Cape Rodney. (Photo: M. Godfrey)
Microalgae are tiny, free-floating marine plants. They are the ocean’s primary producers and form the basis of marine food webs.

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Hoe Chang, Ken Richardson, Michael Uddstrom, and Matt Pinkerton combined ground observations and satellite remote sensing to track algal blooms on the northeast coast of New Zealand in 2002.

The dramatic appearance of a ‘red tide’ algal bloom at Leigh, near Cape Rodney. (Photo: M. Godfrey)

Microalgae are tiny, free-floating marine plants. They are the ocean’s primary producers and form the basis of marine food webs. When conditions are right (for example, optimal light, favourable water temperatures, plentiful nutrients), these microscopic algae can grow rapidly and build up to very high concentrations in a matter of days. This population explosion is commonly referred to as an algal bloom.

Most blooms are harmless and contribute to ocean primary productivity, but a few algal species can be harmful. The build-up of these species, known as a harmful algal bloom (HAB), can damage marine ecosystems and communities. Toxins produced by these harmful species sometimes kill a wide range of marine life, and can lead to illness and death in humans. Shellfish contaminated by harmful species cannot be harvested, and this has negative consequences for the aquaculture industry.

Since the 1993 major toxic shellfish events in New Zealand, shellfish industries and the government regulatory authorities conduct regular monitoring. Water samples are tested for HAB species and shellfish collected from discrete sites are screened for toxicity.

The view from space

Microalgae absorb sunlight for photosynthesis through photo-pigments such as chlorophyll. As algal biomass increases, the colour of the deep ocean under clear skies changes from blue to green because the chlorophyll pigments absorb blue light. Variations in the particular combination of photo-pigments between species can cause other subtle changes in water colour, giving it a hint of red, brown, or cream. The build-up of photo-pigments in the ocean can be detected using satellite-borne ocean-colour sensors such as SeaWiFS (the Sea-viewing Wide Field-of-view Sensor). Ocean-colour satellites measure the intensity of several different colours of light emerging from the sea, giving valuable information about the development and trajectory of blooms over a very large area in real time.

Sea surface temperature (SST) data from space satellites add another dimension to our understanding of the relationships between physical environment and onset of algal bloom events. SSTs are derived from infrared (or thermal) emissions from the ocean surface; the data let us form a high-resolution, synoptic (snapshot) view of upper-ocean structure in real time. At NIWA we have an archive of these data that extends from 1993 to the present.

The 2002 HAB events

When several huge HABs occurred in New Zealand waters in October 2002, NIWA scientists used satellite data to track the events. Most importantly, we also made shipboard measurements to identify the dominant species and provide further information about environmental conditions during bloom events.

From the water: identifying the culprits

Study area and sampling locations. The coloured dots show where blooms were dominated by Karenia (red dots) and Rhizosolenia (blue dot). (Click for detail)

In the Hauraki Gulf during October 2002, tens of thousands of dead fish washed up on beaches at Orewa and Whangaparaoa, north of Auckland. Around the same time, a large number of abalone was reported dead at a marine farm in Kennedys Bay on the eastern coast of Coromandel Peninsula outside the Hauraki Gulf. In all these locations we detected high concentrations of Karenia species, including a newly described species, K. concordia.

Algal cells viewed through the microscope. (Click for enlargement and description)

Members of the public also reported several patches of red surface discoloration. We found that most of these visible blooms were dominated by Noctiluca scintillans, a harmless, non-photosynthetic dinoflagellate species of alga. Noctiluca was not immune to the October 2002 toxic outbreaks, and the organisms died after ingesting cells of Karenia species.

During the same period, there were blooms outside the Hauraki Gulf dominated by Rhizosolenia (diatoms) and Noctiluca, but in this case we detected no Karenia species. Healthy Noctiluca cells were discovered in the region, feeding mainly on diatoms and the larvae of several marine organisms, with a small number feeding on cysts from Alexandrium cf. catenella, an algal species that produces paralytic shellfish poison.

From the sky: satellite observations

Ocean colour

Ocean colour images from September to December 2002 showed the build-up of several patches of high-chlorophyll water along the North Island northeast coast. In the Hauraki Gulf, the build-up apparently started in late September. Map A (above) shows elevated chlorophyll concentrations covering a large area stretching from Waiheke Island inside the Hauraki Gulf to Little Barrier Island at the entrance in the north. Between early and mid October, this high-chlorophyll patch of water coincided with areas where bloom proportion of harmful Karenia species and marine life kills were reported, providing some evidence about the extent of this bloom in the Gulf. Although Noctiluca scintillans also bloomed simultaneously with Karenia species, its lack of chlorophyll makes it difficult to see from space.

Satellite images show ocean colour and sea surface temperature. (Click for enlargement and explanation)

Sea surface temperature

SST data retrieved from the US National Space Administration for the same period provide some insight into the physical environment before the initiation of the HABs. In the late winter of 2002, signs of strong upwelling and deep mixing were observed to extend from the open coastline to the entrance of Hauraki Gulf. At this point no bloom was observed. As seasonal warming progressed, upwelled water inshore started to stabilise. From September onwards, SSTs derived from the satellite showed ‘tongues’ of relatively warm surface waters intruding into the cold, presumably nutrient-rich, nearshore waters close to the entrance of Hauraki Gulf (see map B). We hypothesise that Karenia species originating in offshore water were introduced as seed stock during an incursion into this nutrient-rich coastal region, thereby initiating the 2002 HAB at the entrance of the Gulf.

Potential applications

This study indicates that, in combination with sea-truthing, ocean-colour and sea-surface-temperature data from satellites can be used to continuously monitor bloom events over large areas. The combination of ground and space observations provides much more information than fixed-point monitoring, and is particularly useful for understanding bloom formation and movement over large areas of coastline.

We are currently trying to determine whether it is possible to use the information from satellite observations to distinguish bloom events by colour. This is a difficult task, usually impossible for most individual species, but worth pursuing for taxonomic groups of species, since it would significantly improve bloom-monitoring capability and provide additional information for studies of algal dynamics over large areas.

Further reading

Chang, F.H.; Ryan, K. (2004). Karenia concordia sp. nov. (Gymnodiniales, Dinophyceae), a new nonthecate dinoflagellate isolated from the New Zealand northeast coast during the 2002 harmful algal bloom events. Phycologia 43: 552–562.

Useful links

SeaWiFS: oceancolor.gsfc.nasa.gov/SeaWiFS

NOAA HAB forecast system: www.noaanews.noaa.gov/stories2004/s2323.htm

Dr Hoe Chang’s work focuses on biodiversity, biosecurity, biotechnology, and ocean ecosystems. Dr Ken Richardson, Dr Michael Uddstrom, and Dr Matt Pinkerton are remote-sensing scientists. The authors all work at NIWA in Wellington.

This work was funded by the FRST research programmes ‘Ocean Ecosystems’, ‘Biodiversity and Biosecurity’, and ‘Remote Sensing of Fisheries’. The authors thank the SeaWiFS Project and the Goddard Earth Sciences Data and Information Services Center/Distributed Active Archive Center in Greenbelt, MD, for the data.

Author contact: [email protected]

Teachers’ resource for NCEA AS: Biology 90164 (1.4), 90167 (1.7), 90716 (3.4); Science 90732 (3.6). See other curriculum connections at www.niwa.co.nz/pubs/wa/resources

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