Collusion, Co-Optation, or Evasion: The Politics of Drug Trafficking Violence in Central America

2022 ◽  
pp. 001041402110662
Author(s):  
Laura R. Blume

Why do drug traffickers sometimes decide to use violence, but other times demonstrate restraint? Building on recent work on the politics of drug violence, this article explores how Central American drug trafficking organizations’ strategies impact their use of violence. I argue that three inter-related political factors—corruption, electoral competition, and the politicization of the security apparatus—collectively determine the type of relationship between traffickers and the state that will emerge. That relationship, in turn, determines the primary strategy used by traffickers in that country. Drawing on over two years of comparative ethnographic fieldwork in key transshipment points along the Caribbean coast of Central America, I show how co-optation strategies in Honduras have resulted in high levels of violence, evasion strategies in Costa Rica have produced moderate levels of violence, and collusion strategies in Nicaragua have generated the lowest levels of drug-related violence.

2021 ◽  
Author(s):  
Hugo G. Hidalgo ◽  
Eric J. Alfaro ◽  
Franklin Hernández-Castro ◽  
Paula M. Pérez-Briceño

<p>Tropical cyclones are one of the most important causes of disasters in Central America. Using historical (1970–2010) tracks of cyclones in the Caribbean and Pacific basin, we identify critical path locations where these low-pressure systems cause the highest number of floods in a set of 88 precipitation stations in the region. Results show that tropical cyclones from the Caribbean and Pacific basin produce a large number of indirect impacts on the Pacific slope of the Central American isthmus. Although the direct impact of a tropical cyclone usually results in devastation in the affected region, the indirect effects are more common and sometimes equally severe. In fact, the storm does not need to be an intense hurricane to cause considerable impacts and damage. The location of even a lower intensity storm in critical positions of the oceanic basin can result in destructive indirect impacts in Central America. The identification of critical positions can be used for emergency agencies in the region to issue alerts of possible flooding and catastrophic events.</p>


Author(s):  
Robinson Herrera

Far from monolithic, the seven Central American countries—Belize, Costa Rica, El Salvador, Guatemala, Honduras, Nicaragua, and Panama—each have unique cultural traditions and historical trajectories. Their different geographies, while not deterministic in any facile manner, influenced their development in ways that continue to shape their national characteristics. The cataclysmic 16th-century Spanish Conquest introduced new peoples and cultural traditions to the region. African slaves, primarily from the sub-Saharan region, accompanied the first Spanish ventures, and, later, as the colonies consolidated and grew, peoples of African descent, both enslaved and free, became a part of the area’s economic and cultural landscape. Starting in the late 18th century, African peoples from the Caribbean—whether forcefully exiled or as a result of searching for economic opportunities—traveled to Central America. Despite a contemporary collective historical amnesia that imagines Africans isolated in specific regions, namely the Caribbean coast, peoples of African descent can be found throughout the Central American nations. Rather than addressing each country, a thematic approach that focuses on the Spanish Conquest, slavery, emancipation, the ethnogenesis of African connected cultures, the historical erasure of Africans, and the contributions of peoples of African descent helps to understand the complex ways that peoples of African descent have impacted the history of modern Central America. For far from isolated to small populations along the Caribbean, the African presence can be discerned throughout the region, even in places often perceived as entirely devoid of its influence.


2016 ◽  
Author(s):  
Ana María Durán-Quesada ◽  
Luis Gimeno ◽  
Jorge Amador

Abstract. A climatology of moisture sources linked with Central American precipitation was computed based upon Lagrangian trajectories for the analysis period 1980–2013. The response of the annual cycle of precipitation in terms of moisture supply from the sources was analysed. Regional precipitation patterns are mostly driven by moisture transport from the Caribbean Sea (CS). Moisture supply from the Eastern Tropical Pacific (ETPac) and Northern South America (NSA) exhibits a strong seasonal pattern but weaker compared to CS. The regional distribution of rainfall is largely influenced by a local signal associated with surface fluxes during the first part of the rainy season, whereas large scale dynamics forces rainfall during the second part of the rainy season. The Caribbean Low Level Jet (CLLJ) and the Chocó Jet (CJ) are the main conveyors of regional moisture, being key to define the seasonality of large scale forced rainfall. Therefore, interannual variability of rainfall is highly dependent of the regional LLJs to the atmospheric variability modes. The El Niño-Southern Oscillation (ENSO) was found to be the dominant mode affecting moisture supply for Central American precipitation via the modulation of regional phenomena. Evaporative sources show opposite anomaly patterns during warm and cold ENSO phases, as a result of the strengthening and weakening, respectively, of the CLLJ during the summer months. Trends in both moisture supply and precipitation over the last three decades were computed, results suggest that precipitation trends are not homogeneous for Central America. Trends in moisture supply from the sources identified show a marked north-south seesaw, with an increasing supply from the Caribbean Sea to northern Central America. Long term trends in moisture supply are larger for the transition months (March and October). This might have important implications given that any changes in the conditions seen during the transition to the rainy season may induce stronger precipitation trends.


1957 ◽  
Vol 11 (1) ◽  
pp. 41-54 ◽  
Author(s):  
Norman J. Padelford

For more than a century intellectuals and statesmen in Central America have kept alive a Bolivarian dream of fashioning a political unity in the isthmian region of the Americas. The formation of the Organization of Central American States in 1951 marked a signal accomplishment along a pathway strewn with many obstacles and previous frustrations. The establishment of this organization added a third regional grouping to the two already present in the Americas— the Organization of American States and the Caribbean Commission. It remains to be seen to what extent the three will be able to work together when questions affecting interests of the hemisphere as a whole arise.


Atmosphere ◽  
2020 ◽  
Vol 11 (10) ◽  
pp. 1123
Author(s):  
Hugo G. Hidalgo ◽  
Eric J. Alfaro ◽  
Franklin HernÃandez-Castro ◽  
Paula M. Pérez-Briceño

Tropical cyclones are one of the most important causes of disasters in Central America. Using historical (1970–2010) tracks of cyclones in the Caribbean and Pacific basin, we identify critical path locations where these low-pressure systems cause the highest number of floods in a set of 88 precipitation stations in the region. Results show that tropical cyclones from the Caribbean and Pacific basin produce a large number of indirect impacts on the Pacific slope of the Central American isthmus. Although the direct impact of a tropical cyclone usually results in devastation in the affected region, the indirect effects are more common and sometimes equally severe. In fact, the storm does not need to be an intense hurricane to cause considerable impacts and damage. The location of even a lower intensity storm in critical positions of the oceanic basin can result in destructive indirect impacts in Central America. The identification of critical positions can be used for emergency agencies in the region to issue alerts of possible flooding and catastrophic events.


2017 ◽  
Vol 8 (1) ◽  
pp. 147-161 ◽  
Author(s):  
Ana María Durán-Quesada ◽  
Luis Gimeno ◽  
Jorge Amador

Abstract. A climatology of moisture sources linked with Central American precipitation was computed based upon Lagrangian trajectories for the analysis period 1980–2013. The response of the annual cycle of precipitation in terms of moisture supply from the sources was analysed. Regional precipitation patterns are mostly driven by moisture transport from the Caribbean Sea (CS). Moisture supply from the eastern tropical Pacific (ETPac) and northern South America (NSA) exhibits a strong seasonal pattern but weaker compared to CS. The regional distribution of rainfall is largely influenced by a local signal associated with surface fluxes during the first part of the rainy season, whereas large-scale dynamics forces rainfall during the second part of the rainy season. The Caribbean Low Level Jet (CLLJ) and the Chocó Jet (CJ) are the main conveyors of regional moisture, being key to define the seasonality of large-scale forced rainfall. Therefore, interannual variability of rainfall is highly dependent of the regional LLJs to the atmospheric variability modes. The El Niño–Southern Oscillation (ENSO) was found to be the dominant mode affecting moisture supply for Central American precipitation via the modulation of regional phenomena. Evaporative sources show opposite anomaly patterns during warm and cold ENSO phases, as a result of the strengthening and weakening, respectively, of the CLLJ during the summer months. Trends in both moisture supply and precipitation over the last three decades were computed, results suggest that precipitation trends are not homogeneous for Central America. Trends in moisture supply from the sources identified show a marked north–south seesaw, with an increasing supply from the CS Sea to northern Central America. Long-term trends in moisture supply are larger for the transition months (March and October). This might have important implications given that any changes in the conditions seen during the transition to the rainy season may induce stronger precipitation trends.


2018 ◽  
Vol 676 (1) ◽  
pp. 135-151 ◽  
Author(s):  
Gabriella E. Sanchez ◽  
Sheldon X. Zhang

The violence afflicting the Mexican migration corridor has often been explained as resulting from the brutal takeover of migrant smuggling markets by organized crime, specifically Mexican drug trafficking organizations (DTOs). Through the testimonies of twenty-eight migrants who traveled with smuggling facilitators on their journeys into the United States and who interacted with drug traffickers during their transit, we argue that the metamorphosis taking place may be even more radical, involving the proliferation of actors with little or no criminal intent to operate along the migration trails. Far from market coalescence, the increasing flattening of criminal markets along the migration trail and the proliferation of individuals struggling to survive is the result of increasingly limited paths toward mobility and is not attributable to feared cartels or traficantes alone. The interactions among clandestine actors are not only likely to become more common but also to reflect flexibility and adaptation that hierarchical DTOs cannot explain.


2020 ◽  
Vol 44 (1) ◽  
pp. 278-300
Author(s):  
L. Delgat ◽  
R. Courtecuisse ◽  
E. De Crop ◽  
F. Hampe ◽  
T.A. Hofmann ◽  
...  

Species of the ectomycorrhizal genus Lactifluus, and often entire sections, are typically unique to a single continent. Given these biogeographic patterns, an interesting region to study their diversity is Central America and the Caribbean, since the region is closely connected to and often considered a part of the North American continent, but biogeographically belong to the Neotropical realm, and comprises several regions with different geologic histories. Based on a multi-gene phylogeny and morphological study, this study shows that Central America, Mexico and the Caribbean harbour at least 35 Lactifluus species, of which 33 were never reported outside of this region. It was found that species from the Caribbean generally show affinities to South American taxa, while species from the Central American mainland generally show affinities to Northern hemispheric taxa. We hypothesise that host specificity and/or climate play a crucial role in these different origins of diversity. Because of these different affinities, Caribbean islands harbour a completely different Lactifluus diversity than the Central American mainland. The majority of species occurring on the islands can be considered endemic to certain islands or island groups. In this paper, detailed morphological descriptions are given, with a focus on the unique diversity of the islands, and identification keys to all hitherto described Lactifluus species occurring in Central America and the Caribbean are provided. One new section, Lactifluus sect. Nebulosi, and three new species, Lactifluus guadeloupensis, Lactifluus lepus and Lactifluus marmoratus are described.


1990 ◽  
Vol 32 (1) ◽  
pp. 119-136 ◽  
Author(s):  
Anthony J. Payne

Within the international politics of the Caribbean Basin attention is only rarely paid to the position of Belize. This neglect is the more remarkable since Belize epitomizes — more precisely than any other territory of the region — the characteristic geopolitical problem of the Caribbean caught, as it were, uneasily between the United States, Latin America and Europe. Yet, despite being threatened by the Guatemalan claim to sovereignty over its territory, which delayed its independence until 1981, Belize has skillfully taken advantage of its British colonial past to carve out for itself a distinctive geopolitical space in Central America and the Caribbean. This has allowed it not only to remain relatively undisturbed by the conflicts which have riven the other states of the Central American isthmus, but also to display a commitment to democratic change strong enough to sustain the electoral defeat — in December 1984 — of a regime which had held power in the country for more than thirty years, as well as the defeat of its successor — in September 1989 — after just one term in office.


2019 ◽  
Author(s):  
Richard Styron ◽  
Julio García-Pelaez ◽  
Marco Pagani

Abstract. A database of ~250 active fault traces in the Caribbean and Central American regions has been assembled to characterize the seismic hazard and tectonics of the area, as part of the GEM Foundation's Caribbean and Central American Risk Assesment (CCARA) project. The dataset is available in many vector GIS formats, and contains fault trace locations as well as attributes describing fault geometry and kinematics, slip rates, data quality and uncertainty, and other metadata as available. The data is public and open-source (available at https://github.com/GEMScienceTools/central_am_carib_faults), will be updated progressively as new data is available, and is open to community contribution. The active fault data show deformation in the region to be centered around the margins of the Caribbean plate. Northern Central America has sinistral and reverse faults north of the sinistral Motagua-Polochic Fault Zone, which accommodates sinistral Caribbean-North American relative motion. The Central American Highlands extend east-west along a broad array of normal faults, bound by the Motagua-Polochic Fault Zone in the north and dextral faulting in the southwest between the Caribbean plate and the Central American forearc. Faulting in southern Central America is complicated, with trench-parallel reverse and sinistral faults. The northern Caribbean-North American plate boundary is sinistral offshore of Central America, with transpressive stepovers through Jamaica, southern Cuba and Hispaniola. Farther east, deformation becomes more contractional closer to the Lesser Antilles subduction zone, with minor extension and sinistral shear throughout the upper plate, accommodating oblique convergence of the Caribbean and North American plates.


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