central american isthmus
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Forests ◽  
2021 ◽  
Vol 12 (8) ◽  
pp. 1057
Author(s):  
William J. Harvey ◽  
Gillian Petrokofsky ◽  
Nathan Stansell ◽  
Sandra Nogué ◽  
Leo Petrokofsky ◽  
...  

An ever-increasing demand for agriculture while conserving biodiversity, maintaining livelihoods, and providing critical ecosystem services is one of the largest challenges for tropical land management across the Central American Isthmus today. Climatic and anthropogenic drivers threaten to cause changes in the forest cover and composition for this region, and therefore, understanding the dynamics of these systems and their variability across space and through time is important for discerning current and future responses. Such information is of value especially for risk mitigation, planning, and conservation purposes. The understanding of the forests, water, and land use for this region through time is currently limited, yet it is essential for understanding current patterns of change, particularly with reference to: (i) forest fragmentation; (ii) water availability; and (iii) land management. Through the examination of biotic (e.g., pollen, diatoms, and Sporormiella) and abiotic (e.g., δ 18O, CaCO3, and magnetic susceptibility) proxies, extracted from environmental archives, evidence for longer-term environmental changes can be inferred and linked to drivers of change including climate, burning, and human activities. Proxy environmental data from terrestrial depositional archives across the Central American Isthmus were identified and mapped following best practice for systematic evidence synthesis. Results from the evidence base were summarised to show the spatial and temporal extent of the published datasets. A total of 12,474 articles were identified by a comprehensive search in three major bibliographic databases. From these, 425 articles were assessed for relevance at full-text, and 149 fully met inclusion criteria for the review. These articles yielded 648 proxy records in 167 study sites that were mapped on an interactive map with filters to allow full exploration of the evidence base. Just under half of the studies were published in the last decade. Most studies extracted their data from lake sediments, with a focus on moist tropical forests in lowland sites in Guatemala, Belize, and Mexico. The largest data gaps in the evidence base are Honduras, Nicaragua, Panama, and El Salvador. There are also significant evidence gaps for dry tropical forests, coniferous forests, mangroves, and grasslands. Most of the studies assessed had methodological or presentational limitations that make future meta-analysis difficult and significantly affect the ability to draw conclusions that are helpful for future decision-making. A degree of standardisation, transparency, and repeatability in reporting would be beneficial to harness the findings of the existing evidence base and to shape future research in this geographical area. The systematic map of the evidence base highlights six key review topic areas that could be targeted, if the raw data could be obtained, including: (i) dating uncertainty and standardising reporting; (ii) land use change across space and time; (iii) dispersal pathways of agriculture; (iv) the role and impacts of fire and burning; (v) changes in hydro-climate, water availability, and the risk of tropical storms; and (vi) forest resilience and recovery.


2021 ◽  
Author(s):  
◽  
◽  

2020 was an unprecedented year for Central America and the Dominican Republic. The effect of the global COVID-19 pandemic, exacerbated by the impact of Hurricanes Eta and Iota in some countries, caused the greatest economic contraction the region has undergone in its recent history - surpassing the debt crisis of the 1980s and the international financial crisis of 2009. In 2020, the IDB Group helped the countries in the region respond to these emergencies through approvals that exceeded US$ 4,900 million and disbursements of more than US$ 4,327 million, both reaching historical records. This report highlights the Groups main activities in Central America and the Dominican Republic in 2020 at the regional and country level.


Evolution ◽  
2020 ◽  
Author(s):  
Jose Avila‐Cervantes ◽  
Carlos Arias ◽  
Miryam Venegas‐Anaya ◽  
Marta Vargas ◽  
Hans C. E. Larsson ◽  
...  

Author(s):  
Ricardo Sánchez‐Murillo ◽  
Germain Esquivel‐Hernández ◽  
José L. Corrales‐Salazar ◽  
Laura Castro‐Chacón ◽  
Ana M. Durán‐Quesada ◽  
...  

Authorea ◽  
2019 ◽  
Author(s):  
Ricardo Sanchez Murillo ◽  
Germain Esquivel Hern ndez ◽  
Jos Corrales Salazar ◽  
Laura Castro Chac n ◽  
Ana Dur n Quesada ◽  
...  

Author(s):  
Ricardo Sánchez-Murillo

Numerous socio-economic activities depend on the seasonal rainfall and groundwater recharge cycle across the Central American Isthmus. Population growth and unregulated land use changes resulted in extensive surface water pollution and a large dependency on groundwater resources. This chapter uses stable isotope variations in rainfall, surface water, and groundwater of Costa Rica, Nicaragua, El Salvador, and Honduras to develop a regionalized rainfall isoscape, isotopic lapse rates, spatial-temporal isotopic variations, and air mass back trajectories determining potential mean recharge elevations, moisture circulation patterns, and surface water-groundwater interactions. Intra-seasonal rainfall modes resulted in two isotopically depleted incursions (W-shaped isotopic pattern) during the wet season and two enriched pulses during the Mid-Summer Drought and the months of the strongest trade winds. Notable isotopic sub-cloud fractionation and near-surface secondary evaporation were identified as common denominators within the Central American Dry Corridor. Groundwater and surface water isotope ratios depicted the strong orographic separation into the Caribbean and Pacific domains, mainly induced by the governing moisture transport from the Caribbean Sea, complex rainfall producing systems across the N-S mountain range, and the subsequent mixing with local evapotranspiration, and, to a lesser degree, the eastern Pacific Ocean fluxes. Groundwater recharge was characterized by a) depleted recharge in highland areas (72.3%), b) rapid recharge via preferential flow paths (13.1%), and enriched recharge due to near-surface secondary fractionation (14.6%). Median recharge elevation ranged from 1,104 to 1,979 m a.s.l. These results are intended to enhance forest conservation practices, inform water protection regulations, and facilitate water security and sustainability planning in the Central American Isthmus.


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