纵向数据分析中测地线趋势的非参数聚合。

Kristen M Campbell, P Thomas Fletcher
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引用次数: 2

摘要

我们提出了一种分析纵向成像数据的技术,该技术使用微分同构测地线回归来模拟个体变化,并将这些测地线聚集成非参数组平均趋势。我们的模型是专门为纵向成像研究的不平衡和稀疏特征量身定制的。也就是说,每个人在短时间内测量的数据点很少,而研究人群作为一个整体跨越了很宽的年龄范围。我们使用测地回归来估计个体趋势,这是一个适当的模型,用于捕获在短时间窗口内的形状变化,因为通常在个体中发现。测地线还擅长处理个体内的低样本量,并且可以模拟两个时间点之间的变化。然而,测地线在模拟长期趋势方面是有限的,在这种情况下,匀速可能不合适。因此,我们开发了一种新的非参数回归,将个体趋势汇总为平均群体趋势。我们证明了我们的方法在捕获海马体积(实值数据)的非测地线组趋势和从纵向OASIS数据的全3D MRI的微分对称配准方面的能力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Nonparametric Aggregation of Geodesic Trends for Longitudinal Data Analysis.

Nonparametric Aggregation of Geodesic Trends for Longitudinal Data Analysis.

Nonparametric Aggregation of Geodesic Trends for Longitudinal Data Analysis.

Nonparametric Aggregation of Geodesic Trends for Longitudinal Data Analysis.

We propose a technique for analyzing longitudinal imaging data that models individual changes with diffeomorphic geodesic regression and aggregates these geodesics into a nonparametric group average trend. Our model is specifically tailored to the unbalanced and sparse characteristics of longitudinal imaging studies. That is, each individual has few data points measured over a short period of time, while the study population as a whole spans a wide age range. We use geodesic regression to estimate individual trends, which is an appropriate model for capturing shape changes over a short time window, as is typically found within an individual. Geodesics are also adept at handling the low sample sizes found within individuals, and can model the change between as few as two timepoints. However, geodesics are limited for modeling longer-term trends, where constant velocity may not be appropriate. Therefore, we develop a novel nonparametric regression to aggregate individual trends into an average group trend. We demonstrate the power of our method to capture non-geodesic group trends on hippocampal volume (real-valued data) and diffeomorphic registration of full 3D MRI from the longitudinal OASIS data.

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