scispace - formally typeset
Open AccessJournal ArticleDOI

Dryland climate change: Recent progress and challenges

Reads0
Chats0
TLDR
In this paper, a review describes recent progress in dryland climate change research, showing that the long-term trend of the aridity index (AI) is mainly attributable to increased greenhouse gas emissions while anthropogenic aerosols exert small effects but alter its attributions.
Abstract
Drylands are home to more than 38% of the world's population and are one of the most sensitive areas to climate change and human activities. This review describes recent progress in dryland climate change research. Recent findings indicate that the long-term trend of the aridity index (AI) is mainly attributable to increased greenhouse gas emissions while anthropogenic aerosols exert small effects but alter its attributions. Atmosphere-land interactions determine the intensity of regional response. The largest warming during the last 100 years was observed over drylands and accounted for more than half of the continental warming. The global pattern and inter-decadal variability of aridity changes are modulated by oceanic oscillations. The different phases of those oceanic oscillations induce significant changes in land-sea and north-south thermal contrasts, which affect the intensity of the westerlies and planetary waves and the blocking frequency, thereby altering global changes in temperature and precipitation. During 1948-2008, the drylands in the Americas became wetter due to enhanced westerlies, whereas the drylands in the Eastern Hemisphere became drier because of the weakened East Asian summer monsoon. Drylands as defined by the AI have expanded over the last sixty years and are projected to expand in the 21st century. The largest expansion of drylands has occurred in semi-arid regions since the early 1960s. Dryland expansion will lead to reduced carbon sequestration and enhanced regional warming. The increasing aridity, enhanced warming and rapidly growing population will exacerbate the risk of land degradation and desertification in the near future in developing countries.

read more

Citations
More filters

Response of the zonal mean atmospheric circulation to El Nino versus global warming

TL;DR: In contrast to the strengthening and contraction of the Hadley cell and the equatorward shift of the tropospheric zonal jets in response to El Nino forcing, the hadley cell weakens and expands poleward, and the jets move poleward in a warmed climate, despite the projected “El Nino-like” enhanced warming over the equatorial central and eastern Pacific.

The impact of global land-cover change on the terrestrial water cycle

TL;DR: In this article, the extent of land-cover change caused by people is analyzed. But the authors focus on the terrestrial water cycle and do not consider the effects of human impacts on it.
Journal ArticleDOI

Climate Change and Drought: a Perspective on Drought Indices

TL;DR: In this paper, a formulation of drought indices without considering the factors that govern the background state may lead to drought artifacts under a warming climate, and a formulation based on the energy budget framework can be a better approach compared to only temperature-based equations.

Short-term modulation of Indian summer monsoon rainfall by West Asian dust

TL;DR: In this paper, an analysis of satellite data and global climate model simulations suggests that dust aerosol levels over the Arabian Sea, West Asia and the Arabian Peninsula are positively correlated with the intensity of the Indian summer monsoon.
Journal ArticleDOI

Climate Change and Drought: a Precipitation and Evaporation Perspective

TL;DR: In this article, the effects of greenhouse gas (GHG)-induced global warming may lead to increased surface aridity and more droughts in the twenty-first century due to decreased precipitation in the subtropics and increased evaporative demand associated with higher vapor pressure deficit under warmer temperatures.
References
More filters
Journal ArticleDOI

Natural evaporation from open water, bare soil and grass

TL;DR: It is shown that a satisfactory account can be given of open water evaporation at four widely spaced sites in America and Europe, the results for bare soil receive a reasonable check in India, and application of theresults for turf shows good agreement with estimates of evapolation from catchment areas in the British Isles.

The relationship of drought frequency and duration to time scales

TL;DR: The definition of drought has continually been a stumbling block for drought monitoring and analysis as mentioned in this paper, mainly related to the time period over which deficits accumulate and to the connection of the deficit in precipitation to deficits in usable water sources and the impacts that ensue.
Journal ArticleDOI

Catastrophic shifts in ecosystems.

TL;DR: Recent studies show that a loss of resilience usually paves the way for a switch to an alternative state, which suggests that strategies for sustainable management of such ecosystems should focus on maintaining resilience.
Related Papers (5)
Trending Questions (1)
What are the main environmental challenges facing semi-arid regions?

The main environmental challenges facing semi-arid regions include increasing aridity, enhanced warming, and the risk of land degradation and desertification.