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Jennifer Marohasy

Jennifer Marohasy

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Archives for July 22, 2007

Government Misrepresents Extent of Land Clearing: A Note from Ian Mott

July 22, 2007 By Ian Mott

The latest satellite (SLATS) data on Queensland clearing is now available and it provides an interesting insight into how data can be presented in a way that is quite remote from the truth on the ground. The report, Landcover Change in Queensland 2004-2005 can be seen at www.nrw.qld.gov.au/slats

The annual average area cleared in the period was 351,000ha of which 172,000ha (49%) was remnant vegetation with the remaining 179,000ha (51%) being non-remnant woody regrowth. When this was broken down into Carnahan vegetation classes some 193,000ha (55%) was of a type that would not be included within the meaning of forest under the National Forest Inventory. That is, it was “Tussocky or Tufted Grasses” and other vegetation types that have less than 10% foliage cover and are less than 2 metres tall. This presentation still does not allow us to determine what proportion of the 158,000ha (44.7%) cleared remnant vegetation was actually non-forest vegetation types that may actually benefit from tree removal to restore the grassland/shrub ecosystems.

The report has fine tuned a previous practice of breaking the data into relevant grid squares with a colour code to indicate the area of land cleared in each square. Previous reports have used 30′ X 30′ (Lat/Long) grid cells that covered an area of approximately 280,000 hectares with codes indicating cleared area from <100ha to >5000ha for each cell. This produced a map with numerous lurid dark tones but which told us very little, other than the fact that somewhere within a square measuring 53km by 53km was somewhere between 0.01km2 and 50km2 of clearing.

This has now been broken up into 7’30” X 7’30” (Lat/Long) grid cells that cover approximately 17,500 hectares but these still retain the same colour codes for the same cleared area categories and produce a map with lots of little coloured squares that give the appearance of widespread clearing activity. These can be seen at Figure 8 P18 of the current report.

But the most interesting aspect of this presentation is what it does not tell us about the clearing. The graphic below is an enlargement of a 700,000 hectare scene to the west of Charleville which is recorded as one of the hotbeds of clearing in 2004-2005.

The lower presentation is an enlargement of the SLATS Report while the upper presentation indicates the information that is readily available and could be incorporated into the presentation if the political masters were willing to provide a budget for the truth.

Each of the grid squares has been broken up into 700 smaller squares of 25 hectares each (25 across and 28 down) so we are able to show the actual area of pasture, remnant, and woody regrowth in each grid cell. This then enables one to show each years clearing activity in the respective proportions of regrowth and remnant clearing. More importantly, it allows the viewer to gain an understanding of the relevance of that clearing in relation to the local landscape. Obviously, a large amount of clearing in a cell with a low level of remnant (eg. at E2 below) is of more concern than a cleared fence line in a cell with 75% woody remnant vegetation cover.

When the actual clearing is presented in direct spatial proportion to the area of the grid cell and the area of woody vegetation, we get a much more honest appreciation of what is taking place.

Charleville Remnant B.jpg

Of the approximately 3,450 grid cells indicating clearing activity in the report, more than 3,300 of them were in the two least cleared categories, showing cleared areas from 0 <100ha and 100 <500ha in each cell. The remaining 147 cells were easier to count and, after allocating a modal value in each class, we were able to determine that approximately half of all clearing, some 175,000ha, was cleared from these few cells. After allowing for a modal value of 300ha in the second lowest category and a roughly estimated proportion of 9% (or 300) of the 3300 remaining cells being in the second lowest category this indicated that another 90,000ha of clearing took place in the second lowest category. And this left only about 86,000ha of clearing taking place on the remaining 3000 cells at an average area of only 28 hectares per cell.

When that 28ha of clearing is proportionately represented on our improved data presentation below it would occupy just one of the 700 small squares in the cell. And when viewed in proper proportion it then becomes clear that the overwhelming majority of the scenes where some clearing has taken place, that clearing is of extremely marginal ecological impact. Indeed, it is at a level that would be barely detectable with the naked eye.

But it is in the allocation of this clearing (or current absence of it) between remnant and non-remnant at the grid cell level that provides the real “smoking gun” of systematic institutional deception. This is because a 28ha clearing event on an inland property is more than likely to be either fodder harvesting for stock or clearing for a fence line etc. And we know that mulga pulling for stockfeed is done on a long term rotational basis of 15 to 25 years. And that interval is more than sufficient for past regrowth to return to remnant status, being more than 70% of “normal” height. This provides grounds for informed speculation as to what proportion of remnant clearing, the assumed worst impact, is actually concentrated in small events of minimal consequence while the major events are primarily of non-remnant woody weeds.

We won’t actually know for sure unless we demand that this information, that is already at hand, be presented in a manner that properly informs the community. Anything less is serious misrepresentation by omission.

Ian Mott

Filed Under: Opinion Tagged With: Rangelands, Weeds & Ferals

Radiative forcing due to land use change in southwest Australia

July 22, 2007 By Paul

Having seen Ian Mott’s note on land change, I though I would post this paper suggesting that climate models and therefore the IPCC underestimate the effects of land use change on climate:

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, D09117, doi:10.1029/2006JD007505, 2007

Observational estimates of radiative forcing due to land use change in southwest Australia

Abstract

Radiative forcing associated with land use change is largely derived from global circulation models (GCM), and the accuracy of these estimates depends on the robustness of the vegetation characterization used in the GCMs. In this study, we use observations from the Clouds and Earth’s Radiant Energy System (CERES) instrument on board the Terra satellite to report top-of-the-atmosphere (TOA) radiative forcing values associated with clearing of native vegetation for agricultural purposes in southwest Australia. Over agricultural areas, observations show consistently higher shortwave fluxes at the TOA compared to native vegetation, especially during the time period between harvest and planting. Estimates using CERES observations show that over a specific area originally covered by native vegetation, replacement of half the area by croplands results in a diurnally averaged shortwave radiative forcing of approximately −7 W m−2. GCM-derived estimates for areas with 30% or more croplands range from −1 to −2 W m−2 compared to observational estimate of −4.2 W m−2, thus significantly underestimating radiative forcing due to land use change by a factor of 2 or more. Two potential reasons for this underestimation are incorrect specification of the multiyear land use change scenario and the inaccurate prescription of seasonal cycles of crops in GCMs.

Received 12 May 2006; accepted 22 November 2006; published 15 May 2007.

Keywords: Australia; land use change; radiative forcing.

http://www.agu.org/pubs/crossref/2007/2006JD007505.shtml

Filed Under: Uncategorized Tagged With: Climate & Climate Change

The Little Ice Age in Australia

July 22, 2007 By Paul

I have previously posted comments about this paper, published in the Journal of Quaternary Science that provides evidence for the generally cooler period known as the Little Ice Age being a global phenomenon rather than being limited to the Northern Hemisphere:

Five centuries of climate change in Australia: the view from underground

Henry N. Pollack 1 *, Shaopeng Huang 1, Jason E. Smerdon 2
1Department of Geological Sciences, University of Michigan, Ann Arbor, Michigan, USA
2Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York, USA

Published Online: 27 Sep 2006

Keywords
palaeoclimate • borehole temperatures • Australia

Summary and conclusions

We have analysed 57 borehole temperature profiles from across Australia to reconstruct a ground surface temperature history for the past five centuries. The five-hundred-year reconstruction is characterised by a temperature increase of approximately 0.5 K, with most of the warming occurring in the 19th and 20th centuries. The 17th century was the coolest interval of the five-century reconstruction, perhaps representing a muted expression of the Little Ice Age widely observed in the Northern Hemisphere. Because most of the boreholes were logged prior to 1976, the observed subsurface temperatures do not show the strong warming experienced by Australia in the last two decades of the 20th century. Comparison of the geothermal reconstruction to the high-quality Australian annual SAT (Surface Air Temperature) time series in their period of overlap shows excellent agreement. The full geothermal reconstruction also shows excellent agreement with the low-frequency component of dendroclimatic reconstructions from Tasmania and NewZealand. The warming of Australia over the past five centuries has been about two-thirds that experienced by southern Africa, and only about half that experienced by the continents of the Northern Hemisphere in the same time interval.

This paper provides evidence for different regional responses to global climate change and illustrates the fact that the world has warmed since the end of the LIA, with half of the warming occurring in the 20th century.

Filed Under: Uncategorized Tagged With: Climate & Climate Change

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Jennifer Marohasy Jennifer Marohasy BSc PhD has worked in industry and government. She is currently researching a novel technique for long-range weather forecasting funded by the B. Macfie Family Foundation. Read more

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