Monitoring dynamics of Kyagar Glacier surge and repeated draining of Ice-dammed lake using multi-source remote sensing.

Glacier surges, a primary factor contributing to various glacial hazards, has long captivated the attention of the global glaciological community. This study delves into the dynamics of Kyagar Glacier surging and the associated drainage features of its Ice-dammed lake, employing high temporal resolution optical imagery. Our findings indicate that the surge on Kyagar Glacier began in late spring and early summer of 2014 and concluded during the summer of 2016. This surge resulted in the transfer of 0.321 ± 0.012 km3 of glacier mass from the reservoir zone to the receiving zone, leading to the formation of an ice-dammed lake at the glacier's terminus. The lake experienced five outbursts between 2015 and 2019, with the largest discharge occurring in 2017. And the maximum water depth during this period was 112 ± 11 m, resulting in a water storage volume of (158.37 ± 28.32) × 106 m3. On the other hand, our analysis of the relationship between glacier surface velocity and albedo, coupled with an examination of subglacial dynamics, revealed that increased precipitation during the active phase of the Kyagar Glacier results in accumulation of mass in the upper glacier. This accumulation induces changes in basal shear stress, triggering the glacier's transition into an unstable state. Consequently, glacier deformation rates escalate, surface crevasses proliferate, potentially providing conduits for surface meltwater to infiltrate the glacier bed. This, in turn, leaded to elevated basal water pressure, initiating glacier sliding. Furthermore, we postulated that the repetitive drainage of Kyagar Ice-dammed lake was primarily influenced by the opening and closing of subglacial drainage pathways and variations in inflow volumes. Future endeavors necessitate rigorous field observations to enhance glacier surge simulations, deepening our comprehension of glacier surge mechanisms and mitigating the impact of associated glacial hazards.

Overview of terrestrial water storage changes over the Indus River Basin based on GRACE/GRACE-FO solutions.

Water resources are under severe stress in the highly populated Indus River Basin due to the increased consumption of water across different sectors and climate change. Coping with these challenges, requires a clear understanding on hydrological processes and anthropogenic activities, and how these are influencing recharging and spatiotemporal availability of groundwater in the basin. The present study aims to investigate the natural and anthropogenic impact on Terrestrial Water Storage (TWS) over the Indus River Basin by using a series of statistical methods and the observation data from the Gravity Recovery and Climate Experiment (GRACE) and Follow-On (GRACE-FO). Our results show that (i) TWS Anomaly (TWSA) experienced a significant decrease from 2002 to 2020, particularly in the MUIP; (ii) the UIB showed a weak decreasing trend in TWSA as a result of the accelerated glacier melting; (iii) there was significant loss of groundwater (1.57 mm/month) caused by ineffective water management and over-exploitation; and (iv) assisted by favorable meteorological conditions, the precipitation presented a positive trend against the weakness of the Westerlies, which exerted the positive influence on TWSA.

[Expression of reconstructed BCR-ABL-pIRES-SEA plasmids in the skeletal muscles of BALB/c mice].

This paper is aimed to investigate the transcription and expression of BCR-ABL-pIRES-SEA fusion gene vaccines in vivo in mice. The reconstructed plasmids (BCR-ABL-pIRES-SEA) which were developed previously in our laboratory were injected into the skeletal muscles of BALB/c mice at 14d intervals for three cycles. The transcription and expression of BCR-ABL and staphylococcal enterotoxin A (SEA) in injection site were detected using RT-PCR and immunohistological methods. The BCR-ABL/SEA mRNA and protein could be identified in the injection site of BCR-ABL-pIRES-SEA vaccinated mice. The reconstructed BCR-ABL-pIRES-SEA plasmids can effectively express gene production in the skeletal muscles of mice and have the common features of DNA vaccine.

[Effect of superantigen SEA on the CD3epsilon chain expression on cord blood mononuclear cells stimulated by K562 cells].

AIM: To explore the effect of staphylococcal enterotoxin A(SEA) on CD3(epsilon) chain expression on mononuclear cells in cord blood, which were stimulated by K562 cells. METHODS: The anti-CD3 antibodies(mAb), K562 cells, SEA or both SEA and K562 cells were cocultured with mononuclear cells (MNCs) from four normal human cord blood for 48 hours respectively, Real-time PCR with SYBR Green I technique was used to detect expressed level of CD(epsilon) on MNCs in cord blood and set up a blank control group. Relative changes in expression level of CD3(epsilon) chain were indicated by the 2(-deltadeltaCt); method between each group and the control group. beta2-microglobulin gene(beta2M) was used as an endogenous reference. RESULTS: The expressed level of CD3(epsilon) chain on MNCs was slightly decreased in K562 cell group and were increased in the anti-CD3 antibodies mAb group, SEA group, both of SEA and K562 cell group respectively. The expressed level of CD3(epsilon) chain in both SEA and K562 group was significantly higher than that in the SEA group(P<0.01). CONCLUSION: Superantigen SEA can enhance the expressed level of CD3(epsilon) chain on MNCs stimulated by K562 cells.