Jinda Wang

Effects of the interplanetary magnetic field on the twisting of the magnetotail: Global MHD results

We used the global magnetohydrodynamic (MHD) simulation to investigate effects of the interplanetary magnetic field (IMF) on the twisting of the magnetotail. It is shown that the cross section of the magnetotail is elongated along a certain direction close to the IMF orientation. The elongated direction twists with the IMF orientation, magnitude, and the distance away from Earth, and the quantitative relationship has been given. In addition, the current sheet has a similar twisting behavior as the magnetotail magnetopause, with a smaller twisting angle. Our simulated results fall within the range that people have deduced from observations.

The chain response of the magnetospheric and ground magnetic field to interplanetary shocks

In response to interplanetary (IP) shocks, magnetic field may decrease/increase (negative/positive response) in nightside magnetosphere, while at high latitudes on the ground it has two-phase bipolar variations: preliminary impulse and main impulse (MI). Using global MHD simulations, we investigate the linkage between the MI phase variation on the ground and the magnetospheric negative response to an IP shock. It is revealed that although the two phenomena occur at largely separated locations, they are physically related and form a response chain. The velocity disturbances near the flanks of the magnetopause cause the magnetic field to decrease, resulting in a dynamo which thus powers the transient field-aligned currents (FACs). These FACs further generate a pair of ionospheric current vortex, leading to MI variations on the ground. Therefore, we report here the intrinsic physically related chain response of the magnetospheric and ground magnetic field to IP shocks, and thus link the magnetospheric sudden impulse (SI) and ground SI together.

Effects of Wetland Reclamation on Soil Nutrient Losses and Reserves in Sanjiang Plain, Northeast China

The carbon (C), nitrogen (N) and phosphorus (P) variations of a temperate wetland soil under continuous cultivation for 40 yr were determined and evaluated in the Sanjiang Plain, Northeast China. The results showed that the soil organic carbon (SOC) and total nitrogen (TN) contents in each soil layer decreased sharply after cultivation for 2-3 yr, and exhibited minor differences after cultivation for 11 yr, which showed an exponential decline curve with the increase of cultivation years. The reduction rates of carbon and nitrogen reserves were 14.79% and 28.53% yr−1 at the initial reclamation stages of 2-3 yr and then decreased to 2.02-3.08% yr−1 and 1.98-2.93% yr−1 after cultivation for 20 yr, respectively. Soil total phosphorus (TP) reserves decreased within cultivation for 5 yr, and then gradually restored to the initial level after cultivation for 17 yr. Both SOC and TN could be restored slightly when the farmland was left fallow for 8 yr after reclamation for 11 yr, whereas TP had no significant difference. These results demonstrated that wetland cultivation was one of the most important factors influencing on the nutrient fate and reserves in soil, which could lead to the rapid nutrient release and slow restoration through abandon cultivation, therefore protective cultivation techniques preventing nutrients from loss should be immediately established after wetland reclamation.

A three‐dimensional high Mach number asymmetric magnetopause model from global MHD simulation

The numerical results from a physics-based global magnetohydrodynamic (MHD) model are used to examine the effect of the interplanetary magnetic field (IMF), solar wind dynamic pressure, and dipole tilt angle on the size and shape of the magnetopause. The subsolar magnetopause is identified using the plasma velocity and density, the cusps are identified using the thermal pressure, and the whole shape of the magnetopause is determined with the three-dimensional streamlines traced through the simulation domain. The magnetopause surface obtained from the simulations is fitted with a three-dimensional surface function controlled by ten configuration parameters, which provide a description of the subsolar magnetopause, the cusp geometry, the flaring angle, the azimuthal asymmetry, the north-south asymmetry, and the twisting angle of the magnetopause. Effects of the IMF, solar wind dynamic pressure, and dipole tilt angle on the configuration parameters are analyzed and fitted by relatively simple functions. It is found that the solar wind dynamic pressure mainly affects the magnetopause size; the IMF mainly controls the magnetopause flaring angle, azimuthal asymmetry, and twisting angle; and the dipole tilt angle mainly affects the magnetopause north-south asymmetry and the cusp geometry. The model is validated by comparing with available empirical models and observational results, and it is demonstrated that the new model can describe the magnetopause for typical solar wind conditions.

Exploring the anthropogenic driving forces of China's provincial environmental impacts

Human activities can have dramatic effects on the environment so that evaluating the anthropogenic driving forces is an important issue in the consideration of how humans impact the world. In this paper, ecological footprint (EF) was used as an aggregate index of total human impacts in 31 provinces in mainland China during 2010. The STIRPAT model was employed to analyze the major anthropogenic drivers of EF. The empirical results demonstrate that great disparities of EF exist at the spatial scale. Provinces with the largest total EF are mostly distributed in the populated east coast of China, whereas provinces with the lowest total EF are mostly found in west China. Similar to EF, ecological deficit (ED) is a dominant characteristic of most municipal areas in China. The results of STIRPAT show that population has the largest potential effect on the Chinese environment at the provincial scale, followed by EF intensity, affluence, percentage of gross domestic product (GDP) from the industrial sector, age structure, and per capita land area. Urbanization has negative effects on EF disparities, but it is not an inevitable factor in this case. This study is helpful to recognizing the human effects on environment and helps to facilitate the management of sustainable development across China.

Evaluation of the eco-environmental frangibility in west Jilin Province based on the matter-element model

The west Jilin Province is a typical area in the ecotone between agriculture and animal husbandry, with a frangible eco-environment. With respect to the three aspects of water resource, natural disasters and land degradation, 10 indices were selected to establish a matter-element model for the assessment of eco-environmental frangibility in the west Jilin Province. The results indicate that during 1985-2000, Qian’an, Fuyu, and Changling had the least frangibility (level I), followed by Da’an and Qianguo (level II), and Taobei, Zhenlai, Taonan, and Tongyu had the highest frangibility (level III). On the whole, the counties in Songyuan city were less frangible than those in Baicheng city. Different counties had different frangibilities to environmental factors, e.g., Da’an and Tongyu were frangible in water resource conditions; Taobei, Zhenlai, Taonan, Tongyu and Qian’an suffered most from natural disasters; while Taobei, Taonan and Qianguo were threatened by severe land degradation.