Abstract In this study, we made a review about carbon stocks and fluxes in Mexican freshwater wetlands. Data for carbon storage in roots, soil and biomass have been reported for marshes, forested wetlands and flooded grasslands in southeast Mexico: Veracruz, Chiapas and Yucatan. The largest carbon stock in freshwater wetlands is in the soil (150 Mg C ha-1 a 650 Mg C ha-1) and the forested wetlands showed the highest values. The carbon stock in the biomass ranges from 10 Mg C ha-1 to 162 Mg C ha-1, and forested wetlands showed the highest values. Carbon fluxes measured as litter fall have been reported for forested wetlands in Veracruz (6 Mg C ha-1 year-1 a 9 Mg C ha-1 year-1) only. Methane and carbon dioxide fluxes ranged from 0.01 mg C m-2 d-1 to 1244 mg C m-2 d-1, and 0.009 g C m-2 d-1 to 11 g C m-2 d-1 respectively for Veracruz and Tabasco wetlands. Such carbon fluxes increased up to ten times, when wetlands are transformed to grasslands. It is concluded that the number of publications and study sites on carbon dynamics in Mexican freshwater wetlands is still very small. Therefore, it is necessary to increase the research in this area and enact laws that protect these important carbon sinks. | Resumen Este trabajo hace una revisión bibliográfica sobre los almacenes y flujos de carbono en humedales de agua dulce en México. Se encontraron datos sobre almacenes de carbono en suelo, biomasa aérea y raíces en humedales herbáceos (popales, tulares y carrizales), humedales arbóreos (selvas inundables y palmares) y en humedales transformados en potreros que aún se inundan, para tres estados del sureste mexicano: Veracruz, Yucatán y Chiapas. El mayor almacén de carbono se ha registrado para el suelo de las selvas inundables (150 Mg C ha-1 a 650 Mg C ha-1). Los almacenes de carbono en la biomasa área de las selvas inundables fueron de 10 Mg C ha-1 a 162 Mg C ha-1, siendo también los valores más altos. Con respecto a los flujos de carbono medidos como caída de hojarasca en selvas inundables, solo se encontraron datos para Veracruz (6 Mg C ha-1 año-1 a 9 Mg C ha-1 año-1). Los flujos de metano y bióxido de carbono estuvieron en el intervalo de 0.01 mg C m-2 d-1 a 1244 mg C m-2 d-1 y 0.009 g C m-2 d-1 a 11 g C m-2 d-1 respectivamente, para Veracruz y Tabasco, y dichas emisiones aumentan hasta 10 veces en humedales transformados en potreros. Se concluye que aún son muy pocas las publicaciones y pocos los sitios estudiados sobre la dinámica del carbono en humedales de agua dulce, por lo que hay que incrementar la investigación en esta línea, ya que los humedales son importantes sumideros de carbono y es necesaria una legislación que proteja las reservas de carbono en estos ecosistemas.

This study investigates the occurrence of greenhouse gases (GHGs) and the role of groundwater as an indirect pathway of GHG emissions into surface waters in a gaining stretch of the Triffoy River agricultural catchment (Belgium). To this end, nitrous oxide (N₂O), methane (CH₄) and carbon dioxide (CO₂) concentrations, the stable isotopes of nitrate, and major ions were monitored in river and groundwater over 8 months. Results indicated that groundwater was strongly oversaturated in N₂O and CO₂ with respect to atmospheric equilibrium (50.1 vs. 0.55 μg L⁻¹ for N₂O and 14,569 vs. 400 ppm for CO₂), but only marginally for CH₄ (0.45 vs. 0.056 μg L⁻¹), suggesting that groundwater can be a source of these GHGs to the atmosphere. Nitrification seemed to be the main process for the accumulation of N₂O in groundwater. Oxic conditions prevailing in the aquifer were not prone for the accumulation of CH₄. In fact, the emissions of CH₄ from the river were one to two orders of magnitude higher than the inputs from groundwater, meaning that CH₄ emissions from the river were due to CH₄ in-situ production in riverbed or riparian zone sediments. For CO₂ and N₂O, average emissions from groundwater were 1.5 × 10⁵ kg CO₂ ha⁻¹ year⁻¹ and 207 kg N₂O ha⁻¹ year⁻¹, respectively. Groundwater is probably an important source of N₂O and CO₂ in gaining streams but when the measures are scaled at catchment scale, these fluxes are probably relatively modest. Nevertheless, their quantification would better constrain nitrogen and carbon budgets in natural systems.

Combined simulation-optimization modeling is an essential tool for coastal groundwater management. However, determining the appropriate simulation-optimization approach for specific seawater intrusion problems remains a significant challenge, especially for the real-world conditions associated with management of complex groundwater systems, competing management objectives, and global concerns of future climate change. In this study, a linked multi-objective simulation-optimization framework, the MOSWTGA (multi-objective optimal code, coupling SEAWAT and an improved genetic algorithm), was applied to a coastal groundwater system in Zhoushuizi district of Dalian City in northern China. The system has fractured karst aquifers and is modelled for the next 20 years (from 2010) under the moderate greenhouse gas concentration scenario RCP4.5 (representative concentration pathways) in the CNRM (Centre National de Recherches Météorologiques) and MIROC (Model for Interdisciplinary Research on Climate) climate modes derived from the Coupled Model Intercomparison Project Phase 5 (CMIP5). The MOSWTGA was developed by integrating the density-dependent groundwater flow and solute transport code SEAWAT with a genetic algorithm improved by adding the Pareto-dominated ranking module, Pareto solution set filter, and fitness sharing procedure. A set of near Pareto-optimal solutions of the trade-off between the maximum of the total pumping rate and the minimum of the extent of seawater intrusion was obtained. The study tried to provide a theoretical basis for real-world groundwater management under the given conditions.

This report presents the World Bank Group's experience in climate and disaster resilient development and contends that it is essential to eliminate extreme poverty and achieve shared prosperity by 2030. The report argues for closer collaboration between the climate resilience and disaster risk management communities through the incorporation of climate and disaster resilience into broader development processes. Selected case studies are used to illustrate promising approaches, lessons learned, and remaining challenges all in contribution to the loss and damage discussions under the United Nations Framework Convention on Climate Change (UNFCCC). The introduction provides an overview of the UNFCCC and also introduces key concepts and definitions relevant to climate and disaster resilient development. Section two describes the impacts of globally increasing weather-related disasters in recent decades. Section three summarizes how the World Bank Group's goals to end extreme poverty and boost shared prosperity are expected to be affected by rising disaster losses in a changing climate. Section four discusses the issue of attribution in weather-related disasters, and the additional start-up costs involved in climate and disaster resilient development. Section five builds upon the processes and instruments developed by the climate resilience and the disaster risk management communities of practice to provide some early lessons learned in this increasingly merging field. Section six highlights case studies and emerging good practices in climate and disaster resilient development. Section seven concludes the report, summarizing key lessons learned and identifying potential gaps and avenues for future work. | En el informe “Crear resiliencia mediante la integración de los riesgos climáticos y de desastre en el proceso de desarrollo” se muestra por qué es esencial desarrollar la resiliencia al clima para poder alcanzar los objetivos del Grupo del Banco Mundial de poner fin a la pobreza extrema y promover la prosperidad compartida. En este resumen ejecutivo se hace un llamado a la comunidad internacional del desarrollo a trabajar en diversas disciplinas y sectores con el propósito de generar una mayor resiliencia de largo plazo, reducir los riesgos y evitar mayores costos en el futuro. Se hace hincapié en la necesidad de crear instituciones y dotarlas de los medios para emprender la continua labor que se requiere para lograr un desarrollo en que se tenga en cuenta la resiliencia al clima y a los desastres. Al destacar las mejores prácticas, el informe muestra cómo los instrumentos financieros y los programas de intervención, sumados a la experiencia y conocimientos especializados en preparación para casos de desastre adquiridos durante décadas, están ayudando a las naciones a prepararse para un mundo más expuesto a los cambios. Asimismo, en el informe se reconoce que un desarrollo con tales características tiene costos iniciales adicionales, que se amortizan en el largo plazo si se actúa correctamente. En este contexto, el informe propugna una colaboración más estrecha entre las comunidades responsables de crear resiliencia al clima y las encargadas de administrar los riesgos de desastre, y la incorporación de la resiliencia al clima y a los desastres en los procesos de desarrollo en sentido más amplio. Presenta estudios de casos seleccionados para mostrar algunos enfoques promisorios, las lecciones aprendidas y los desafíos que aún existen. | Le présent rapport explique pourquoi le renforcement de la résistance aux chocs climatiques est une condition essentielle à la réalisation des objectifs du Groupe de la Banque mondiale — mettre fin à la pauvreté extrême et promouvoir une prospérité partagée — et pourquoi il devrait constituer la clé de voûte du programme mondial de développement. À défaut d’aider les pays, les régions et les villes pauvres et vulnérables à se préparer et à s’adapter aux risques climatiques actuels et futurs, nous risquons de mettre en péril des décennies d’acquis du développement. Nous espérons que ce rapport, en s’appuyant sur l’expérience de la Banque mondiale en matière de résistance aux chocs climatiques et de préparation aux catastrophes naturelles, contribuera utilement au débat international en cours sur les moyens de lutte contre les pertes et les dommages occasionnés par le changement climatique. Le rapport reconnaît cependant qu’un tel développement exige au départ des financements supplémentaires qui s’avéreront rentables à long terme si les choses sont faites correctement. Dans ce contexte, le rapport préconise un renforcement de la collaboration entre les collectivités engagées dans l’application de mesures de résistance aux chocs climatiques et de gestion des risques de catastrophe, ainsi que l’intégration de ces mesures dans le cadre plus large de leurs processus de développement. Le rapport s’appuie sur diverses études de cas pour illustrer les démarches prometteuses, les enseignements tirés de l’expérience et les difficultés qui restent à surmonter. Le rapport entend contribuer au débat engagé dans le cadre de la Convention-cadre des Nations Unies sur les changements climatiques au sujet des pertes et des préjudices liés aux effets néfastes des changements climatiques. Il s’adresse principalement aux professionnels du développement et aux décideurs nationaux qui doivent composer avec le défi posé par une aggravation possible des catastrophes causées par l’évolution graduelle des conditions climatiques moyennes et extrêmes.