国际学生入学条件
All official transcripts must be sent directly to the program to which you intend to apply. For a listing of contacts, please visit the program mail stop directory. You may also upload an unofficial transcript directly within your online application.
Rice University accepts transcripts delivered electronically through Parchment. Programs are able to receive transcripts through other online services as well.
Applicants from Chinese institutions can request and submit official transcripts directly through CHESICC. Requests are processed by CHESICC and will be sent electronically to be associated with your application. If submitting through CHESICC you will not need to submit a paper copy of your transcript. Go here to get started.
For 2024 admissions, Rice generally is not requiring the GRE. However, individual degree programs have the option of recommending, strongly recommending, or requiring the general GRE. See the Programs of Study page or reach out to your program of admission for clarification.
In general, applicants should have at least a 3.0 (B) grade point average, or the equivalent, in their undergraduate work.
The TOEFL IBT or IBT Home Edition. A minimum score of 90 is required
IELTS Indicator. A minimum score of 7 is required.
Duolingo. A minimum score of 115 is required.
展开 IDP—雅思考试联合主办方
雅思考试总分
7.0
了解更多
雅思考试指南
- 雅思总分:7
- 托福网考总分:90
- 托福笔试总分:160
- 其他语言考试:Duolingo. A minimum score of 115 is required.
CRICOS代码:
申请截止日期: 请与IDP顾问联系以获取详细信息。
课程简介
我们对控制从太古代到全新世的长期和短期气候与环境变化感兴趣。研究的特殊领域包括冰川-冰川间的气候变化,温室-冰室的振荡,突变的气候,长期和短期的碳循环,大气中的氧气释放,物理和化学风化,地球大气的起源和演变,化学海洋学以及地表,深海,浅层地壳和沉积物中的水-岩石相互作用。我们使用各种工具,包括稳定同位素地球化学,元素地球化学,生物地层学,沉积学和地球物理学,来重建海洋和陆地环境中的过去气候。
Climate System Science research at Rice uses a combination of climate models, paleoclimate proxy data, and new techniques like data assimilation and proxy system modeling to constrain climate changes of the past, present, and future. We work to understand rapid climate transitions in the past to better understand how climate change may impact societies under continued anthropogenic change. For example, water isotopes in climate models and paleoclimate proxy data provide a direct window into how atmospheric circulation (e.g. the Walker and Hadley Circulations) changed in the past, and how it might respond to future warming. In particular, we are interested in Gulf Coast climate resilience & forecasting, tracking incidence of Gulf hurricanes and the atmospheric dynamics that give rise to extreme rainfall over Texas (and, in general, the Americas). Using climate model simulations spanning Last Glacial Maximum, 21,000 years ago, to 2100, we examine the rates, magnitudes, and spatial patterns of climate dynamics on Earth.
展开