Abstract

The Galapagos Islands are a global hotspot of environmental change. However, despite their potentially major repercussions, little is known about current and expected changes in regional terrestrial climate variables and sea surface temperatures (SST). Here, by analysing existing meteorological observations and secondary datasets, we find that the Islands have warmed by about 0.6 °C since the early 1980s, while at the same time becoming drier. In fact, the onset of the wet season is currently delayed 20 days. This drying trend may reverse, however, given that future climate projections for the region suggest mean annual precipitation may increase between 20 and 70%. This would also be accompanied by more extreme wet and hot conditions. Further, we find that regional SST has increased by 1.2 °C over the last two decades. These changes will, in turn, translate into deterioration of marine ecosystems and coral, proliferation of invasive species, and damages to human water, food, and infrastructure systems. Future projections, however, may be overestimated due to the poor capacity of climatic models to capture Eastern-Pacific ENSO dynamics. Our findings emphasize the need to design resilient climate adaptation policies that will remain robust in the face of a wide range of uncertain and changing climatic futures.

Highlights

  • The Galapagos Islands are a global hotspot of environmental change

  • We find that mean annual land surface temperatures over the last 35 years (1981–2017) ranged from 22 °C to about 26 °C as read by the meteorological stations in Santa Cruz and San Cristobal (Fig. 1)

  • We find that the multi-model mean annual precipitation over the two decades would increase between 5% and around 25% across the three islands evaluated, and throughout the overall region (Fig. 3)

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Summary

Introduction

The Galapagos Islands are a global hotspot of environmental change Despite their potentially major repercussions, little is known about current and expected changes in regional terrestrial climate variables and sea surface temperatures (SST). The onset of the wet season is currently delayed 20 days This drying trend may reverse, given that future climate projections for the region suggest mean annual precipitation may increase between 20 and 70%. We find that regional SST has increased by 1.2 °C over the last two decades These changes will, in turn, translate into deterioration of marine ecosystems and coral, proliferation of invasive species, and damages to human water, food, and infrastructure systems. In 2016, the Islands experienced drought conditions resulting from La Niña This delayed the onset of the rainy season, posing difficulties for agricultural activities and overall water supply. Climate changes, along with greater stress on food, water and overall social systems, will have repercussions for the Islands’ natural diversity and conservation strategies

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