Skip to main content

Search the SPREP Catalogue

Refine Search Results

Language

Available Online

Available Online

14 result(s) found.

Sort by

You searched for

  • Available Online Yes
    X
  • Collection Climate Change Resilience
    X
  • Subject Climatic changes
    X
The state of agricultural dommodity markets 2018. agricultural trade, climate change and food security
Environmental Governance, Climate Change Resilience, BRB
Available Online
2018
This edition of The State of Agricultural Commodity Markets focuses on the complex and underexplored intersection between agricultural trade, climate change and food security. It is clear that we cannot tackle hunger without finding adaptation and mitigation solutions to climate change in agriculture and food systems. It is also clear that the uneven impact of climate change across regions and countries, and the corresponding changes in food availability and access will affect international trade patterns and trade routes. This report supports these discussions by providing an in-depth analysis of the Paris Agreement and the WTO agreements to enhance clarity and provide guidance on policy options that could strengthen the mutually supportive role of these accords in tackling climate change and hunger. Wide-ranging policy actions are necessary to ensure that trade will contribute to the efforts aimed at ensuring food security and promoting adaptation and mitigation to climate change. The uneven impact of climate change across the world and its implications for agricultural trade, especially for developing countries, underlines the need for a balanced approach to policies, which should enhance the adaptive role of trade, while supporting the most vulnerable.
Extreme weather: does nature keep up?: observed responses of species and ecosystems to changes in climate and extreme weather events: many more reasons for concern
Climate Change Resilience
Available Online

Leemans, Rik

,

van Vilet Arnold

2004
Plants, birds, insects, mammals, amphibians and fishes are rapidly responding to the observed changes in climate everywhere on the planet. Extreme high temperatures immediately result in hefty responses. The responses, however, significantly differ from species to species and from year to year, which complicates a clear attribution of causes. The ecological impacts are nowadays visible everywhere through changes in the timing of life cycle events and the geographic distributions of species. Plants have advanced flowering by up to 30 days and are now doing so at dates never documented in the last two centuries. Some species show a dramatic increase in range area, disrupting ecosystems like, for example, the rapid spread over millions of hectares of the Mountain Pine Beetle in North America and the northward expansion of the Oak Processionary caterpillar in The Netherlands. Also fires have increased catastrophically in tropical wet forests during the severe droughts of the El Niño years in the nineties. Other species show a dramatic decrease in distribution or population sizes, illustrated by bleaching corals and disappearing amphibians worldwide. Warm winters, hot summers, excessive precipitation and extended droughts are weather events that trigger these responses
Climate change and water: technical paper of the IPCC
Climate Change Resilience, Biodiversity Conservation
Available Online

Bates, Bryson

,

Kundzewicz, Zbigniew

,

Palutikof Jean

,

Wu, Shaohon Wu

2008
Observational records and climate projections provide abundant evidence that freshwater resources are vulnerable and have the potential to be strongly impacted by climate change, with wide-ranging consequences for human societies and ecosystems. Observed warming over several decades has been linked to changes in the large-scale hydrological cycle such as: increasing atmospheric water vapour content; changing precipitation patterns, intensity and extremes; reduced snow cover and widespread melting of ice; and changes in soil moisture and runoff. Precipitation changes show substantial spatial and inter-decadal variability. Over the 20th century, precipitation has mostly increased over land in high northern latitudes, while decreases have dominated from 10°S to 30°N since the 1970s. The frequency of heavy precipitation events (or proportion of total rainfall from heavy falls) has increased over most areas (likely). Globally, the area of land classified as very dry has more than doubled since the 1970s (likely). There have been significant decreases in water storage in mountain glaciers and Northern Hemisphere snow cover. Shifts in the amplitude and timing of runoff in glacier- and snowmelt-fed rivers, and in ice-related phenomena in rivers and lakes, have been observed (high confidence).