The direct and indirect impacts of population growth and economic development on maize (Zea mays L.) diversity in highland Guatemala

This paper discusses the impacts of population growth and economic development on maize diversity in highland Guatemala. In the context of this discussion, economic development specifically refers to the recent expansion of the non-traditional agricultural exports (NTAEs). Population growth and economic development (i.e. NTAEs) are linked because as land has become scarce in highland Guatemala, due to the poor distribution of land resources and rapid population growth over the past 50 years, many farmers have turned to non-traditional economic strategies such as new crops that produce more income per unit of land. These new crops have improved the economic conditions of many farming families, but it has come at a cost regarding the maintenance of local maize varieties and household food security.     

Mapping massacres: GIS and state terror in Guatemala

This paper employs GIS (geographic information systems) technology to visually display the locations of massacres associated with Guatemala’s civil war. While there have been other, more general maps published depicting the spatial dimensions of violence in Guatemala, few other maps depict this information at the department level, nor have they included information on indigenous populations and physical geography.These maps are part of the emerging field of human rights GIS. For example, over the past two decades, maps have become tools of empowerment in Central America and elsewhere, maps usually made with GIS technology. Indigenous groups in many countries in particular have embraced GIS technology and have begun to use maps as tools in their fight for land and marine resources, as well as greater political autonomy. In the case of massacres in Guatemala, displaying exactly where violent acts took place is one way to educate the Guatemalan public regarding the terrible violence of the recent past. Knowing the name of a specific town where a massacre took place is more concrete, potentially leading to perception of place and people, rather than simply being aware of violence in the countryside.     

On the determination of the energy and depth of volcanic explosions (paper dedicated to G. S. Gorshkov)

The determination of the energy and depth of powerful volcanic explosions using direct geophysical and geological methods is rarely successful. In most of cases investigators have to solve the problem of estimating the energy of an explosion, its depth, the mass and the amount of thrown-out materials from the dimensions of the funnel (crater, maar) and from geological data. Experiments with big throw-out blasts have allowed us to determine the energy and depth of explosions by giving us relations which determine the radius of the explosion funnel as a function of the energy of explosion and of the depth of its center (1) $$R_o = F(E,W)$$ whereR _o is the radius of the funnel,E is the energy,W is the depth of the explosion center. The inverse problem — to determineE andW from a knownR _o — has an ambiguous solution and it is solved parametrically relative toE andW. In order to obtain an unambiguous solution, some more or less arbitrary conditions must be assumed. When the problem of volcanic explosions is examined from the outer ballistic point of view the following equation is obtained whereR _t is the throw-out distance of explosion fragments. (2) $$R_1 = F(E,W)$$ Equations (1) and (2) give us an unambiguous determination of the energy of explosionE and of the depth of the centerW. There is a good correlation between these results and the data from direct geophysical observations.     

Neue Wege in die Ökotoxikologie: Quantitative Verhaltensmessungen an Fischen als Toxizitätsendpunkt

New Ways to Ecotoxicology: Quantitative Recording of Behaviour of Fish as Toxicity Endpoint The BehavioQuant system will be introduced which uses the integrative whole-organism response by automatized recording and quantifying the spontaneous behaviour of fish and other test organisms. While moving unrestricted within the test chamber, the movements of each single fish are recorded by video imaging, and their traces are digitized numerically by x-/y-coordinates. From the object traces several test parameters are calculated which give information about behavioural changes of the observed fishes. These various parameters are: the average swimming velocity (motility), the average swimming depth below surface, the inconstancy of motility, the frequency of turns, the standard frequency distributions of vertical and horizontal positions (can be used for quantification of a preference for dark or light habitats), and the distance behaviour. A continuously monitoring of up to 16 aquaria is possible. The statistic comparison between treated groups and control groups is done for each test parameter separately. The automatical evaluation of the continuous observation of surface waters results from a comparison of the actual behaviour data to the data of a reference period. Some examples for the applications of the BehavioQuant system will be demonstrated (effects of atrazine), and their results will be discussed. Behavioural changes of a single species can finally cause changes in biocenotic structures and functions. Therefore, it is necessary to include the results of quantitative behaviour measurements in ecotoxicological hazard assessment.     

On experiments using an auto-regressive moving-average model for predicting the monthly 50–100 kPa thickness anomalies

A series of 75 auto-regressive integrated moving-average (ARIMA) forecasts of monthly mean 100–50 kPa thickness anomalies with lead time of one month are produced for 455 grid points over the northern hemisphere. The results are indistinguishable from persistence forecasts when the scores are averaged over the domain. A more detailed view indicates some differences which may merit closer investigation. Differences in the behaviour of positive and negative anomaly forecasts are also described.Some aspects of the methodology are discussed briefly in the introductory sections. The model used in the experiment is described in detail. A shortcoming of the method is that it does not lend itself to seasonal stratification.     

Land Cover Changes on Ambergris Caye,Belize: A Case Study of Unregulated Tourism Development

Measuring land-use, land-cover change in biodiverse, tropical countries is critical for conservation management and sustainable planning because it provides quantifiable data regarding broad environmental changes. This project uses Landsat satellite imagery to document vegetation cover change on Ambergris Caye, Belize, from 2000 to 2017. The close proximity of the Belize Barrier Reef Reserve System has made Ambergris Caye the most popular tourist destination and economic hub in Belize. As a result, the region has undergone intense commercial and residential development coupled with rapid population growth over the past two decades. Understanding general trends in landscape dynamics is critical for the natural resource–based tourism industry of Belize to continue to thrive. Unsupervised classification methods and a per pixel postclassification comparison were used with Landsat imagery to estimate loss in vegetation cover and increases in urban and barren land. The results indicate a 10.85 percent decrease in vegetation and a 39 percent increase in urban and barren land during the seventeen-year study period with an annual forest loss rate of 0.67 percent per year using a compound interest rate formula. The results of this analysis represent a baseline study of vegetation change on Ambergris Caye to inform management and conservation efforts.     

Paleoindication of acidification in Kleiner Arbersee (Federal Republic of Germany,Bavarian Forest) by chydorids,chrysophytes, and diatoms

In a sediment core of Lake Kleiner Arbersee, located in the Bavarian Forest on gneiss bedrock and with spodosolic soils in the catchment, acidification was reconstructed using assemblages of chydorids, scaled chrysophytes, and diatoms as paleoindicators. All paleoindicators demonstrated acidification of Kleiner Arbersee. There were marked differences, however, in the extent of the indicated acidification: In lower layers, where scaled chrysophytes and chydorids clearly indicate beginning acidification, pH-decline inferred by diatoms lies within the standard deviation, and is statistically not significant until the 7 cm layer. We conclude that mallomonadaceans reflect the acidification of the water body and strongly respond to the lowest seasonal pH, as their indicated rate of acidification is higher than that of diatoms, which appear to more closely indicate the pH of the sediment/water interface, especially when the pH of the water column has dropped below ca. 5.5. Chydorids may additionally be influenced by proton release of dense Sphagnum-stands, which cover the littoral of Kleiner Arbersee completely.We dedicate this paper to Prof. Dipl.-Ing. L. Strobel, who encouraged new perspectives in limnological water management, on the occasion of his 65^th anniversary.     

Stream Interactions and Interplanetary Coronal Mass Ejections at 0.72 AU

We present comprehensive surveys of 203 stream interaction regions (SIRs) and 124 interplanetary CMEs (ICMEs) during 1979 – 1988 using Pioneer Venus Orbiter (PVO) in situ solar-wind observations at 0.72 AU and examine the solar-cycle variations of the occurrence rate, shock association rate, duration, width, maximum total perpendicular pressure (P _t), maximum dynamic pressure, maximum magnetic field intensity, and maximum velocity change of these two large-scale solar-wind structures. The medians, averages, and histogram distributions of these parameters are also reported. Furthermore, we sort ICMEs into three groups based on the temporal profiles of P _t, and we investigate the variations of the fractional occurrence rate of three groups of ICMEs with solar activity. We find that the fractional occurrence rate of magnetic-cloud-like ICMEs declined with solar activity, consistent with our former 1-AU results. This study at 0.72 AU provides a point of comparison in the inner heliosphere for examining the radial evolution of SIRs and ICMEs. The width of SIRs and ICMEs increases by 0.04 and 0.1 AU, respectively, and the maximum P _t decreases to about 1/3 from Venus to Earth orbit. In addition, our work establishes the statistical properties of the solar-wind conditions at 0.72 AU that control the solar-wind interaction with Venus and its atmosphere loss by related processes. Electronic Supplementary Material The online version of this article () contains supplementary material, which is available to authorized users.     

Statistical evaluation of primary relevellings

For the following problems

- estimating the statistical parameters of the precise levelling,

- adjusting the primary levelling networks and

- estimating vertical crustal movements

mathematical models are being sketched out. Results obtained in evaluating primary relevellings in the G.D.R. are reported.