Cover Principle Findings Introduction Methods & Results Data Summry
Discussion/Conclusion Glossary Literature Cited
Figures & Tables 1989/1999 Kelp Bed Maps

Materials and Results

The methodology utilized in this kelp resource inventory, to document the extent of the kelp resource within the MBNMS, was divided into four phases:

  1. Kelp canopy aerial photography,
  2. Qualitative kelp bed canopy mapping,
  3. Quantitative kelp bed canopy/planimeter area and density analysis (1999), and
  4. Quantitative comparison of 1989 and 1999 kelp resource extent within the Monterey Bay National Marine Sanctuary.

The methods utilized in this current survey were similar to those used in the 1989 inventory, to ensure data compatibility and comparability with this and other subsequent studies. Although the defined scope of this study was limited to the measurement of current resource abundance, specific comparisons were made with the last previous systematic analysis (1989), to document short-term changes in kelp canopy extent

1) Kelp Canopy Aerial Photography

A) Kelp canopy Aerial Photoqraphy

The methodoiogy related to obtaining high-quallty Imagery of the tully deveioped 1599 California coastal kelp resource was divided into two sections: 1) survey timing, imaging, and logistic considerations, and 2) photography of the 1999 kelp resource.

1) Survey Timing, Imaging, and Logistic Considerations

The seasonal timing, photographic scale, and flight parameters of this aerial survey were established, as in previous surveys, to systematically obtain imagery that best represented the maximum extent of the current kelp resource. Acceptable "survey windows" were chosen for the aerial over-flights in response to several biologicai (seasonai timing of maximum canopy development), physical (tidal level, weather and sea state) and logistic factors (length of survey range).

Seasonal timing of maximum kelp canopy development was the major biological factor involved in scheduling this resource survey, and established the criteria around which all other iogistic decisions were made. Within California, it has been observed, that the maximum extent of canopy forming kelp species occurs in August through October, with maturity of the Nereocystis canopy determining the beginning of this "biological window", and early season storms determining the end.

Within this three month period, several acceptable "tidal windows" were selected (utilizing NOM tide tables for Monterey and San Simeon) that would allow the aerial imagery to be obtained at tidal levels of less than +1.G' MLLW. Once the tidal windows were established, the actual survey was conducted during the first window that had acceptable associated environmental conditions. These conditions included adequate

ceiling and visibility (>10,000' MSL and five miles), surface winds less than ten knots, sea/sweli less than five feet, and a sun angle of greater than 30 degrees from vertical. In California, changeable weather (especially coastal fog, high winds and sea state) can be a major limiting factor on survey timing, and can frequently reduce the number of acceptable survey days in a given season to less than twenty. During the previous (1989) survey, the aerial imagery was obtained within these optimum biological, tidal, and environmental windows, thereby allowing meaningful comparisons of seasonal kelp resource areal extent.

The aircraft altitude (9,500' MSL) and photographic scale (1"=3,217') used for these surveys was selected to provide a good balance between resource resolution and rendition on the imagery, the selected base-mapping scale (1:24,000), and the overali length of the survey area (276 miles). At this altitude and photographic scale, the entire survey range (Cambria to Rocky Point) could be accurately recorded, under optimum conditions, during two low-tidal periods. Considering the changeabie nature of California coastal weather; this methodology allowed the maximum utiiization of the few optimum survey dates. With regards to resource resoiution on the imagery; ground truth measurements have indicated that the smaiiest kelp "dots" on the 1 :24,000 scale maps (approximately the size of a text "period" from this document), represent as few as six surface stipes from a single Macrocystis kelp plant.

The film used on this survey was 70 mm Kodak color infrared - type 2443, the accepted standard for use in documenting the areal extent of marine surface vegetation. Its ability to increase the contrast between kelp and the surrounding water, without sacrificing resoiutiGn, made it ideal for resource surveys of this type. Despite this abiiity, infrared film does have iimitations regarding its utility in recording sub-surface coastal kelp canopies. Due to its poor water penetration properties of approximateiy two feet (Helgeson 1970); this fiim wiil not record keip stipes that are significantiy puiled beiow the surface due to high winds and seas, high tides, and tidai currents. This especiaiiy affects sparse Nereocystis canopies, which can be compietely submerged by the above factors (especiaiiy tidai currents), and not recorded on the imagery. Carefui attention to survey timing that corresponded with acceptabie winds, seas, and the "time of the low tide" at each coastal location, was necessary to insure accurate canopy rendition on the imagery.

2) Photography of the 1999 Kelp Resource

When the biological, tidal, imaging, and logistic factors were considered together, three possible "optimum survey windows" were established for the 1999 kelp resource inventory: 1) September 24-27, 2) October 7-10, and 3) October 23-27,1999.

Aerial photography of the 1999 kelp resource was accomplished on October 7 and 9, 1999, during the second optimum survey window. Calm winds, low seas, and mostly clear skies were present throughout the survey range on both dates, with the exception of patchy coastal fog from Pt. Sur north to San Francisco on October 7. A summary of associated environmentai conditions, in addition to visual observations taken during the survey were presented in fiqures 1.1 and 1.2.

Continuous, sequential, vertical photographs (20%-30% overlap) were taken from 9,500' MSL (75mm lens) of the coastal zone between Point Estero and Point Sur on October 7, and from Point Sur to Rocky Point on October 9. Approximately 20% shoreline was included on each image to facilitate accurate projection onto the base line maps. Larger canopies, that were not fully recorded on the initial "in-shore" photographic transect, were referenced on parallel "off-shore" flight lines. Each new transect was "side-lapped!' by 30%40% with those in-shore, to facilitate the accurate mapping of these off-shore canopies.

The imagery from each of the survey dates was processed normally, judged of excellent quality, and allowed the complete and subsequent mapping of the coastal kelp canopies within the study range. This indexed imagery was presented as: "California Coastal Kelp Resources - Monterey Bay National Marine Sanctuary Summer 1999 -Aerial SurveY Imaaery" - Binder 1/1 "Bolinas Lagoon to Pt. Estero".

2) Qualitative Kelp Bed Canopy Mapping

Kelp bed mapping was accomplished in two phases: A) base-line map preparation, and B) kelp bed canopy area mapping and indexing.

A) Base-line Map Preparation

The base-line maps for this coastal kelp survey were originally designed for the 19&9 inventory, and subsequently used again in this effort. This base-map series presents an accurate and continuous depiction of the California state coastal zone from the Oregon to the Mexican borders, including southern California offshore islands, and allowed the systematic mapping of the sanctuary-wide resource.

Eighty-three contiguous base-line maps ~24"x36", scale 1:24,000) were made of the California coastal zone using USGS 7 1f2' quadrangle maps (scaie 1:24,000) as a reference. These maps offered extensive shoreline detaii, high accuracy, and continuous coastal coverage for the entire state. Each of the "quad" maps was copied on a calibrated photocopier (Sharp "8400"). The contiguous 'Ishoreline'' portions of each of the map copies were then assembled together, and became the land reference on each of the base maps. All standard detail from these USGS maps was preserved, including prominent shoreline features, offshore rocks, rivers, beaches, rocky intertidal habitat, towns, harbors, and topographic relief. In addition, the CDF&G kelp bed numbering system, which divides the state-wide kelp resource into discrete beds based on bearings from key geographic points, was also included.

The coastal zone, within the MBNMS, from Rocky Point to Cambria Rock, was located on maps 27 - 44 within this map set. These maps were indexed by map number (table 1), and maP name (table 2), and CDF&G numbered kelp beds present on each map page were also included. To aid in orientation and facilitate the "field use" of the maps, prominent ~eo~raphic features were listed alphabetically in tabular form (table 3), with cross-references to the map name and number where they were found.

B) Kelp Bed canoPy Area Mappinq and Indexing

All color infrared slides from the survey were projected onto the base-line maps, and after aligning common shoreline features from each media, individual kelp plants and kelp canopies (see glossary) were hand transferred. The transfer process specifically involved: 1) the visual analysis of the extent of kelp represented on each slide by reference to color and surface appearance, 2) the identification of the "usable" portion of the image that was largely distortion-free (center three-fourths), 3) positioning this "usable" portion of the projected image in its proper location on the base-map, with regard to both shore-line features and kelp from other overlapping imagery, and 4) the black shading of all visible kelp, both developed canopies and individual plants. These black-shaded areas represented the areal extent of the actual kelp plants composing the surface canopy, and areas within the perimeter of the canopy that did not contain kelp were left un-shaded. When fully rendered from the survey imagery, each mapped canopy closely resembled the appearance of the actual surface canopy when viewed from above.

These mapped canopies represented the quaiitative kelP bed canopy area (see glossary) occupied within the survey range, and were presented in Section 4 - "Kelp Bed Canopy Area Maps: 2744" - October 1999 (24"x36", 11"x17", and 8.5"x11"). Similar maps from the 1989 inventory were presented in Section 5 - "Kelp Bed Canopy Area Maps: 27-44" - October 1989 (24"x36", 11"x17", and 8.5"x11") for comparative purposes.

3) Quantitative Kelp Canopy Planimeter Areas and Relative Density Analysis

The quantitative analysis of the sanctuary-wide kelp resource abundance within the MBNMS was divided into three sections: a) analysis of the 1999 MBNMS sanctuary wide coastal keip resource, by CDF&G kelp bed number, b) 'standardization" of the area anaiysis of the 1989 kelp resource inventory dataset, and 3) comparison of the 1999 kelp resource extent with that measured during the 19&9 inventory. Observed iarge-scale changes in resource abundance were presented in the "Gata Summary/Principle Findings" section.

A) Analvsis of the 1999 MBNMS Sanctuarv-wide Coastal Kelp Resource

Quantitative kelp bed canopy and planimeter areas (see giossary) were accurately determined from the maps using computer image processing techniques. Each map page was scanned fuil scaie at 100 dots/inch (dpi) using a "Microtek" 9600 XL flat-bed image scanner. Area values were determined by screen "pixel counting", utilizing "Global Lab Image" (V3.1) image processing software (Data Translation). Kelp bed canopv/planimeter areas and values for the relative densitv index (see glossary) were tabulated by CDF&G kelp bed number, presented in table 4, and plotted in fiqure 2.

B) Standardization of the Area AnalYsis of the 1989 KelP Resource Dataset

As previously described, the 1989 original kelp imagery data were collected under similar parameters utilized in the current study. In addition, the same base-maps and mapping technique were also employed to render the extent of the surface canopy. The computer area analysis, though, did not call for a value for "quantitative canopy area" (the actual numeric extent of the surface kelp canopy) or "relative density indeX', and focused instead only on ~planimeter area", since this was all that had been used in previous surveys. The "qualitative planimeter area" (see glossary), instead of being objectively derived by computer image enhancement, was subjectively derived by CDF&G personnel by manually estimating the kelp canopy perimeter, and assuming 1 OG% kelp coverage within. Although accurate area values were subsequently obtained for the "quantitative planimeter area"; this methodology was not accurately repeatable for comparative purposes in this study.

In response to these limitations, kelp bed canopy area maps numbers 27-44 from the 1989 state-wide kelp resource inventory were scanned, as previously described, and subjected to the same computer area analysis utilized in the current (1999) inventory. Comparison of the total kelp bed planimeter area, utilizing current methodology, with that determined in 1589 yielded a difference of less than 1% (25.814 sq. mi. (1999) vs. 25.631 sq. mi. (1989). Comparisons of area values at the individual "kelp bed" level, though, averaged a difference of 10% from that previousiy determined, further emphasizing the subjective nature of the previous analysis.

The standardized values for 1989 kelp bed canopy/Planimeter areas and the reiative densitY index within the MBNMS, by CDF&G kelp bed number, were presented in table 5, and plotted in fiqure 3.

C) comParisons of the 1989 and 1999 MBNMS Coastal Kelp Resource

Kelp bed canopY/Planimeter areas and values for the relative density index, for both the 1989 and 1999 inventories were presented in Table 6 and plotted in fi~ure 4

In order to evaluate the significance of observed changes in resource extent between the two surveys, a t-test ("paired two sample for means") was applied to the data sets from tables 6. This test evaluates whether a samples' means are distinct, and does not assume equal population variance (Sokal and Rohlf, 1981). This test was judged appropriate, since there was a natural pairing of measurements making up each distinct value for canoPylplanimeter area and RDI. Each data pair were analyzed at the 95% confidence level (p = .05), and the results of the tests were summarized in the "data summary/principle findings" section

All spreadsheet data from tables 1~ are provided in "Excel 95/97" ("XLS" - Microsoft Inc.) file format. The data file, MBNMSK99 XLS, was included on two 3.5" floppy disks, and presented in each of the data binders in Section 6 - Electronic Data.


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