Rodrigues Ariane A, Macedo Marcia N, Silvério Divino V, Maracahipes Leandro, Coe Michael T, Brando Paulo M, Shimbo Julia Z, Rajão Raoni, Soares-Filho Britaldo, Bustamante Mercedes M C
Department of Ecology, University of Brasília, Brasília, Distrito Federal, Brazil.
Woodwell Climate Research Center, Falmouth, Massachusetts, USA.
Glob Chang Biol. 2022 Nov;28(22):6807-6822. doi: 10.1111/gcb.16386. Epub 2022 Sep 8.
The Brazilian Cerrado is one of the most biodiverse savannas in the world, yet 46% of its original cover has been cleared to make way for crops and pastures. These extensive land-use transitions (LUTs) are expected to influence regional climate by reducing evapotranspiration (ET), increasing land surface temperature (LST), and ultimately reducing precipitation. Here, we quantify the impacts of LUTs on ET and LST in the Cerrado by combining MODIS satellite data with annual land use and land cover maps from 2006 to 2019. We performed regression analyses to quantify the effects of six common LUTs on ET and LST across the entire gradient of Cerrado landscapes. Results indicate that clearing forests for cropland or pasture increased average LST by ~3.5°C and reduced mean annual ET by 44% and 39%, respectively. Transitions from woody savannas to cropland or pasture increased average LST by 1.9°C and reduced mean annual ET by 27% and 21%, respectively. Converting native grasslands to cropland or pasture increased average LST by 0.9 and 0.6°C, respectively. Conversely, grassland-to-pasture transitions increased mean annual ET by 15%. To date, land changes have caused a 10% reduction in water recycled to the atmosphere annually and a 0.9°C increase in average LST across the biome, compared to the historic baseline under native vegetation. Global climate changes from increased atmospheric greenhouse gas concentrations will only exacerbate these effects. Considering potential future scenarios, we found that abandoning deforestation control policies or allowing legal deforestation to continue (at least 28.4 Mha) would further reduce yearly ET (by -9% and -3%, respectively) and increase average LST (by +0.7 and +0.3°C, respectively) by 2050. In contrast, policies encouraging zero deforestation and restoration of the 5.2 Mha of illegally deforested areas would partially offset the warming and drying impacts of land-use change.
巴西塞拉多是世界上生物多样性最为丰富的稀树草原之一,然而其原有植被覆盖面积的46%已被开垦,用于种植作物和放牧。这些大规模的土地利用转变(LUTs)预计会通过减少蒸散量(ET)、升高地表温度(LST)并最终减少降水量来影响区域气候。在此,我们将中分辨率成像光谱仪(MODIS)卫星数据与2006年至2019年的年度土地利用和土地覆盖图相结合,量化了塞拉多地区土地利用转变对蒸散量和地表温度的影响。我们进行了回归分析,以量化六种常见土地利用转变对塞拉多景观整个梯度上的蒸散量和地表温度的影响。结果表明,将森林开垦为农田或牧场使平均地表温度升高了约3.5°C,年平均蒸散量分别减少了44%和39%。从木质稀树草原转变为农田或牧场使平均地表温度升高了1.9°C,年平均蒸散量分别减少了27%和21%。将原生草地转变为农田或牧场分别使平均地表温度升高了0.9°C和0.6°C。相反,草地到牧场的转变使年平均蒸散量增加了15%。迄今为止,与原生植被下的历史基线相比,土地变化已导致每年返还到大气中的水分减少了10%,整个生物群落的平均地表温度升高了0.9°C。大气中温室气体浓度增加导致的全球气候变化只会加剧这些影响。考虑到未来的潜在情景,我们发现放弃森林砍伐控制政策或允许合法森林砍伐继续(至少2840万公顷),到2050年将进一步减少年蒸散量(分别减少-9%和-3%),并使平均地表温度分别升高+0.7°C和+0.3°C。相比之下,鼓励零森林砍伐和恢复520万公顷非法砍伐地区的政策将部分抵消土地利用变化带来的变暖和干燥影响。