Category Archives: Tools

Emergent news: a discussion by Kevin Kelly

Kevin Kelly, co-founder of Wired Magazine, author of Out of Control, and former editor of the Whole Earth Review, an early systems and sustainability magazine writes about collaborative web filtering sites. The sites he mentions are interesting for technology news and entertainment, but are not good at international news, environmental and development news, science news, or many of the other types of news that I find interesting. However, the collaborative filtering approaches behind these approaches are quite interesting. Science sites that attempt to do the same thing include Faculty of 1000, which isn’t free but uses reviews by many academics to identify interesting papers in different fields (previously mentioned on this weblog). Nature had a news article Science in the age of the web (Nov 2005) on the slowness of scientists in adopting such tools. Kevin Kelly reviews a bunch of sites and their approaches:

What’s new? Consensus Web Filters

Like a lot of people, I find that the web is becoming my main source of news. Some of the sites I read are published by individuals, but I find the most informative sites are those published by groups of writers/editors/correspondents, including those put out by Main Street Media (MSM). However for the past three months my main source of “what’s new” has been a new breed of website that collaboratively votes on the best links.

This genre does not have an official name yet, but each of these sites supplies readers with pointers to news items that are ranked by other readers. None of these sites generates news; they only point to it by filtering the links to newsy items. Using different formulas they rank an ever moving list of links on the web. The velocity of their lists varies by site, but some will have a 100% turnover in a few days. I check them daily.

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Science, good causes, and bad arguements

Steve Rayner has an editorial in the Feb 2006 issue of Global Environmental Change – What drives environmental policy? about science and public policy. He writes:

Rather than resolving political debate, science often becomes ammunition in partisan squabbling, mobilized selectively by contending sides to bolster their positions. Because science is highly valued as a source of reliable information, disputants look to science to help legitimate their interests. In such cases, the scientific experts on each side of the controversy effectively cancel each other out, and the more powerful political or economic interests prevail, just as they would have without the science. This scenario has played out in almost every environmental controversy of the past 25 years (Sarewitz 2000).

This phenomenon has led to a widespread pathology: the use of bad arguments for good causes.

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Mapping the world by watershed

From World Resources Institute‘s Watersheds of the World (2003) visualizations of some social-ecological properties of the world’s major watershed:

Cropland Area by Basin

Average Population/km2 (1995)

Water availability per person (1995)

The map shows the 114 major watersheds in the world. The map includes the largest transboundary watersheds and small basins that are representative of a particular geographic area. Omitted regions, shown in white, are primarily smaller coastal drainage basins or regions with no permanent rivers (more info).

Thunderstorms and cross-scale land atmosphere couplings

In a Dec 2005 commentary on Feddema et al (2005) The Importance of Land-Cover Change in Simulating Future Climates. Roger Pielke Sr. writes on the role of land use change in shaping thunderstorms:

One example of how land use and land cover affects global climate is the changing spatial and temporal pattern of thunderstorms. Land use and land cover change and variability modify the surface fluxes of heat and water vapor. This alteration in the fluxes affects the atmospheric boundary layer, and hence the energy available for thunderstorms. As shown in the pioneering work of Riehl and Malkus and Riehl and Simpson, at any time there are 1500 to 5000 thunderstorms globally (referred to as “hot towers”) that transport heat, moisture, and wind energy to higher latitudes. Because thunderstorms occur over a relatively small percentage of Earth’s surface, a change in their spatial patterns would be expected to have global climate consequences. The changes in the spatial patterning of thunderstorms result in regional alterations in tropospheric heating that directly change atmospheric and ocean circulation patterns, including the movement and intensity of large-scale high- and low-pressure weather systems. Most thunderstorms (by a ratio of about 10 to 1) occur over land, and so land use and land cover have a greater impact on the climate system than is represented by the fraction of area that the land covers.

NASA has mapped global lighting strikes. The below image shows the global average annual occurrence of lightning at a resolution of ½° by ½°.

Compare this map against Gordon et al’s map of vapour flow changes, and it becomes apparent that some of the areas of strong vapour flow change are in areas of high thunderstorm activity.  It would be interesting to discover what effect the changes in land cover/land use are doing to thunderstorms and if this has any effect on regional/global climate.

Fishing through marine foodwebs

Tim Essington, Anne Beaudreau and John Wiedenmann have a interesting new paper in PNAS Fishing through marine food webs.

The paper elaborates on Pauly and others influential 1998 paper Fishing Down Marine Food Webs that showed that the mean trophic level of global fisheries statistics declined from 1950 to 1994 (from an average of 3.3 to 3.1).

Essington et al analyzed regional fisheries data from 1950 to 2001. They also found a decline in trophic level in 30 of 48 large marine ecosystems, and that the average decline was .42 trophic levels (almost twice as large as the decline found by Pauly et al). However, they did more than replicate Pauly et al’s work at a regional level, they also tested two alternative models of fishing down foodwebs – sequential collapse (the removal of top levels) vs. sequential addition (adding lower level fisheries). They evaluated these models by examining the temporal dynamics of upper-trophic-level fishery catches when fishing down the food web was occurring:

Under the sequential collapse replacement mode, a decline in the mean trophic level should be accompanied by reduced catches of high-trophic-level species as these species become economically extinct. Under the sequential addition mode, however, we expect catches of upper-trophic-level species to be maintained or even increase.

In the 30 large marine ecosystems that exhibited a decline in trophic level , they found 15 that matched the sequential addition model, 6 that showed no pattern, and 9 that showed sequential collapse. They differences between the two models are illustrated in Figure 1 from the paper, shown below.

Fishing down food websFig. 1. Illustrative examples of the sequential collapse replacement (A) and sequential addition (B) mode of fishing down the food web. Total yearly catch for each 0.1 trophic-level increment is indicated by the color bar on the right (104 kg yr 1). The mean trophic level (white line) was smoothed by using a locally weighted regression smoother. (A) The Scotian Shelf ecosystem exhibited a sharp decline in mean trophic level from 1990 to 2001 owing to the collapse of the cod fishery followed by a decline in the herring fishery and then the growth of the northern prawn fishery. (B) The mean trophic level of the Patagonian Shelf declined from 1980 to 2001, during which time catches for upper-trophic-level species (Argentinean hake) grew substantially while new fisheries for shortfin squid developed.

Essington and his coauthors point out that fisheries science, at least in the published literature, has assumed that fishing down food webs follows the sequential collapse model, and this model has different policy implications to the sequential addition model.

Perhaps the most important policy consideration of the sequential addition mode is that, in most ecosystems of the world, several trophic levels are now exploited simultaneously. These diverse fisheries impose conflicting demands on marine ecosystems that are not generally well represented in single-species management plans that do not consider the effects of these alternative fisheries on each other. As the structure of fisheries and the management environment evolve, the scientific community faces a new challenge of conducting broad-scale ecological research to support the development of more holistic, ecologically based approaches to fisheries management.

Another description of the research is provided in a U Washington press release.

Evaluation of ecosystem services provided by multifunctional agriculture in the USA

George Boody and colleagues used a scenario-development exercise to discover that some types of changes in agricultural management can lead to economic benefits as well as improvements in the delivery of multiple ecosystem services.(Boody et al. 2005. Multifunctional agrcitulture in the United States. BioScience 55: 27 – 38.)

The team of 17 members (including farmers, government agency workers, and acadmics from several disciplines) worked with stakeholders in 2 southern Minnesota (USA) watersheds to develop 4 scenarios evaluating the future of agricultural management in the area.

These two watersheds face many of the same issues found in other agricultural regions of the United States: there are fewer farms now than in past decades; farms are growing in size as farmers buy out their neighbors; more land is leased; the diversity of crops is declining; and more land is managed by large companies working on non-contiguous areas, necessitating transport of manure and other items around the region.

The 4 scenarios they developed were (click for maps of landcover in one of the watersheds):

A) continuation of current trends
B) Implementation of BMPs (best management practices)
C) Maximizing diversity and profitability
D) Increased vegetative cover

The team estimated changes in fish populations in each watershed’s streams, greenhouse gas emissions from agriculture, and carbon sequestration in each watershed under the conditions of each scenario. In one watershed, Scenarios B, C, and D all reduced N loading to the Mississippi River by at least 30% (a goal set by the Mississippi River/Gulf of Mexico Nutrient Task Force). In the other watershed, simply implementing BMPs (Scenario B)was not enough to reach this reduction goal.

In addition, the team estimated the short-term economic effects of each of the 4 scenarios, including net farm income, farm production costs, and commodity and CRP payments. Net farm income was greatest in Scenario C or D, depending on the watershed, despite declines in CRP and commodity payments in those scenarios. The authors also estimated externality cost savings due to reduced sedimentation and flooding.

In their conclusions, the authors state (p. 35):

Our analysis indicates that diversifying agriculture on actively
farmed land could provide environmental, social, and
economic benefits.Citizens would be willing to pay for these
benefits.

They also point out the importance of social capital and changes in agricultural policy to the ability to achieve the transitions required to enter Scenario B, C, or D.

More detail about this project can be found in the report here, and more information on other projects related to stewardship of farmland, sustainable agriculture and sustainable communities can be found at the web site of the Land Stewardship Project.

Anthropogenic Modification of Vapours Flows and Tipping Points in the Earth System

Compare the map of soil moisture – atmosphere couplings against Gordon et al’s 2005 map of changes in vapour flows in the Human modification of global water vapor flows from the land surface.

PNAS Vapour Flows

Figure shows spatial distribution of net changes in vapor flows between potential vegetation and actual deforested and irrigated vegetation in mm/yr. The aggregated global change as compared with the potential vegetation is small (400 km3/yr), but the map illustrates the large spatial redistribution of water vapor flows from the land surface at the global scale.

Note that the location of increases in vapor flows in irrigation matches up with several of the hotspots identified in the map of soil moisture – atmosphere couplings – central Great Plains of North America, and India. Change occurs also in less intense hot spots appear in South America and China. Consquently, the combination of these two papers predicts that irrigation should have altered the local climate in these regions more than in other regions.

Leverage Points in the Earth System: Soil Moisture

The 2004 Science paper – Regions of Strong Coupling Between Soil Moisture and Precipitation – by Koster et al. used a dozen independent climate models to estimate ‘hot spots’ on Earth’s surface where precipitation is affected by soil moisture anomalies during Northern Hemisphere summer. They propose that these hot spots are, in a sense, land-surface analogs to the ocean’s “El Niño hot spot” in the eastern tropical Pacific.

Soil moisture is a slowly vary aspect of the Earth system (relative to weather). Soil moisture can persist for months. Soil moisture, influences evaporation and other surface energy fluxes can influence weather.

Soil moisture atmospheric coupling

Figure: Hot spots of soil moisture – local precipitation coupling appear in the central Great Plains of North America, the Sahel, equatorial Africa, and India. Less intense hot spots appear in South America, central Asia, and China.

The hot spots are located in regions that in areas that are at intermediate moisture levels. The authors argue that this is because in wet climates, soil water is plentiful and evaporation is controlled not by soil moisture but by net radiative energy. In dry climates evaporation rates are sensitive to soil moisture but they are small. Consquently the biggest impact of soil moisture on evaporation is in the transition areas between dry and wet climates.

What this analysis suggests is that these hotspots are areas in which changes in land use – especially those that alter soil moisture – such as irrigation or land clearing, will have a larger impact of regional climate.

Anoxic zones – mapping ecosystem tradeoffs (a start)

Current industrial agricultural practices, particularly the overuse of fertilizer and its sloppy management, frequently create a tradeoff between agricultural production and coastal eutrophication. That is increases in agricultural yields have produced low oxygen zones around the world. The UNEP Global Environmental Outlook 2003 maps the location of coastal anoxic zones world wide (somewhat confusingly the worst cases – the persistent ones are coloured yellow, next worst red and orange, and least worst blue).
Global distribution of oxygen-depleted coastal zones.

Global distribution of oxygen-depleted coastal zones. The 146 zones shown are associated with either majorpopulation concentrations or with watersheds that deliver large quantities of nutrients to coastal waters.

Legend:

  • Annual – yearly events related to summer or autumnal stratification
  • Episodic – events occurring at irregularintervals greater than one year
  • Periodic – events occurring at regular intervals shorter than one year
  • Persistent –all-year-round hypoxia

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