Earth System Dynamics
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A 12-year high-resolution climatology of atmospheric water transport over the Tibetan Plateau
Earth System Dynamics - Tập 6 Số 1 - Trang 109-124
Abstract. The Tibetan Plateau (TP) plays a key role in the water cycle of high
Asia and its downstream regions. The respective influence of the Indian and East
Asian summer monsoon on TP precipitation and regional water resources, together
with the detection of moisture transport pathways and source regions are the
subject of recent research. In this study, we present a 12-year high-resolution
cli...
Simulation of observed climate changes in 1850–2014 with climate model INM-CM5
Earth System Dynamics - Tập 9 Số 4 - Trang 1235-1242
Abstract. Climate changes observed in 1850–2014 are modeled and studied on the
basis of seven historical runs with the climate model INM-CM5 under the scenario
proposed for the Coupled Model Intercomparison Project Phase 6 (CMIP6). In all
runs global mean surface temperature rises by 0.8 K at the end of the experiment
(2014) in agreement with the observations. Periods of fast warming in 1920–1940
...
The response of precipitation characteristics to global warming from climate projections
Earth System Dynamics - Tập 10 Số 1 - Trang 73-89
Abstract. We revisit the issue of the response of precipitation characteristics
to global warming based on analyses of global and regional climate model
projections for the 21st century. The prevailing response we identify can be
summarized as follows: increase in the intensity of precipitation events and
extremes, with the occurrence of events of “unprecedented” magnitude, i.e., a
magnitude not f...
Differential climate impacts for policy-relevant limits to global warming: the case of 1.5 °C and 2 °C
Earth System Dynamics - Tập 7 Số 2 - Trang 327-351
Abstract. Robust appraisals of climate impacts at different levels of
global-mean temperature increase are vital to guide assessments of dangerous
anthropogenic interference with the climate system. The 2015 Paris Agreement
includes a two-headed temperature goal: "holding the increase in the global
average temperature to well below 2 °C above pre-industrial levels and pursuing
efforts to limit the...
Global modeling of withdrawal, allocation and consumptive use of surface water and groundwater resources
Earth System Dynamics - Tập 5 Số 1 - Trang 15-40
Abstract. To sustain growing food demand and increasing standard of living,
global water withdrawal and consumptive water use have been increasing rapidly.
To analyze the human perturbation on water resources consistently over large
scales, a number of macro-scale hydrological models (MHMs) have been developed
in recent decades. However, few models consider the interaction between
terrestrial wate...
Gender and climate change in the Indian Himalayas: global threats, local vulnerabilities, and livelihood diversification at the Nanda Devi Biosphere Reserve
Earth System Dynamics - Tập 6 Số 2 - Trang 505-523
Abstract. Global climate change has numerous implications for members of
mountain communities who feel the impacts in both physical and social
dimensions. In the western Himalayas of India, a majority of residents maintain
a livelihood strategy that includes a combination of subsistence or small-scale
agriculture, livestock rearing, seasonal or long-term migration, and localized
natural resource e...
Farmers' perceptions of and adaptation strategies to climate change and their determinants: the case of Punjab province, Pakistan
Earth System Dynamics - Tập 6 Số 1 - Trang 225-243
Abstract. Climate change is a global environmental threat to all economic
sectors, particularly the agricultural sector. Pakistan is one of the countries
negatively affected by climate change due to its high exposure to extreme events
and low adaptive capacity. In Pakistan, farmers are the primary stakeholders in
agriculture and are more at risk due to climate vulnerability. Based on farm
househol...
A trend-preserving bias correction – the ISI-MIP approach
Earth System Dynamics - Tập 4 Số 2 - Trang 219-236
Abstract. Statistical bias correction is commonly applied within climate impact
modelling to correct climate model data for systematic deviations of the
simulated historical data from observations. Methods are based on transfer
functions generated to map the distribution of the simulated historical data to
that of the observations. Those are subsequently applied to correct the future
projections. ...
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