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.
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雅思考试总分
7.0
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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.
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申请截止日期: 请与IDP顾问联系以获取详细信息。
课程简介
赖斯的地球系统科学涉及大气,海洋,生物圈,地球表面及其深层内部之间的地球化学,生物地球化学和物理相互作用。我们的研究重点是在不同的储层之间随时间尺度(从季节到千禧年到十亿年)之间进行质量交换。我们使用各种工具,包括沉积学,地球化学和生物地球化学,以更好地理解这些相互作用在气候变化,生物演化,环境变化以及大气,海洋和地壳的成分演化中的作用。<br>利用冰川沉积物作为过去冰川状况的档案,山冰川到大陆规模冰原的动力学随时间变化。我们的工具是沉积岩心,地震成像和海底测深法。我们特别关注的是南极冰盖,过去几十年几乎
We study the dynamics of mountain glaciers to continental-scale ice sheets as a function of time using glacial sediments as archives of past glacial conditions. Our tools are sediment drill cores, seismic imaging, and seafloor bathymetry. Our particular focus is the Antarctic ice sheet, conducting oceanographic expeditions almost every other year for the last several decades. We also study the composition of the ancient atmosphere using gas bubbles preserved in ice cores.
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