Dimensions of Grace: Factor Analysis of Three Grace Scales

Measuring grace is challenging. Prior research found the Grace Scale (GS), Richmont Grace Scale (RGS), and The Amazing Grace Scale (TAGS) to be reliable, have promising convergent and divergent validity, and to inter-correlate strongly. However, they may tap different constructs, or grace may be multidimensional (Bufford, Blackburn, Sisemore, & Bassett, 2015). Here two exploratory factor analyses of the combined items showed five factors: experiencing God’s grace, costly grace, grace to self, grace from others, and grace to others, partially paralleling Watson, Chen and Sisemore (2011). Items from all three scales loaded on Factor 1, only items from the RGS loaded on Factor 2. The remaining factors were mostly GS items and a few RGS items. The three scales measure somewhat different constructs. Preliminary validity for the five factors is promising. Regressions showed that combinations of the other four proposed scales accounted for at most about one third of the variance on any given grace factor. The five factors showed different patterns of relationships to criterion variables. We propose a 36 item Dimensions of Grace Scale combining items from all three scales for further exploration

GRACE gravity solutions validated by in-situ ocean bottom pressure in different regions of the global ocean

The GRACE satellite mission provides gravity field estimates of the Earth with unprecedented accuracy. Nevertheless,the realistic detection of oceanic mass redistribution remains challenging due to comparatively small signalamplitude, aliasing by tides and other short-term variability, and smoothing of small spatial scales. To verify thecapability of GRACE to measure oceanic mass variability, a validation with in-situ timeseries of Ocean BottomPressure (OBP) timeseries is essential.Here, different GRACE gravity fields provided by the GRACE Science Data System (CSR, GFZ, JPL), GRGS,ITG and others are compared with more than 140 timeseries of OBP sensors deployed throughout all oceans.The performance of the different GRACE products to capture oceanic mass variability is assessed by a weighedcorrelation analysis, taking into account the length and data quality of the in-situ time series. Both Gaussianfiltering and an ocean-model derived spatial pattern filtering method are used for the GRACE data, whereas forthe in-situ timeseries, different de-tiding and de-trending methods are applied to reduce aliasing and sensor drift.The analysis aims (a) to quantify the skill of different GRACE products and to quantify the advances made byrecent GRACE gravity field releases with improved data processing, and (b) to identify regions where GRACEperforms exceptionally well (e.g. high latitudes), and in which parts of the oceans GRACE fails to detect real OBPvariability. Spatial patterns related to the performance of GRACE may help to predict the quality of spacebornegravity measurements also for those oceanic regions where no in-situ data are available. This is critical for thefuture use of GRACE to remotely determine water mass redistribution in all oceans

Kant’s Robust Theory of Grace

In this paper I argue against two prevailing views of Kant’s Religion. Against commentators such as Michalson and Quinn, who have argued that Kant’s project in Religion is riddled with inconsistencies and circularities, I show that a proper understanding of Kant’s views on grace reveals these do not exist. And contra commentators that attribute to Kant at best a minimalist conception of grace, I show that Kant’s view of it is remarkably robust. I argue that Kant works with three different conceptions of grace. These are: a) grace and the God within, b) grace and the transformation of the fundamental orientation, and c) grace that can be laid hold of; the first and the last play a significant role in his philosophy of religion

Grace Upon Grace: living Water

(Excerpt) Two months ago, on February 22, a Lutheran pastor and his wife, both faithful and fruitful servants of our Lord, began their personal celebration of the feast of victory for our God. They now chant with the saints and all the heavenly host. Worthy is Christ the Lamb who was slain, whose blood set us free to be people of God. It would only be just if the choir director had chosen that hymn of praise to be sung by the choir that day, because the two I speak of were the Rev. Herbert and Ruth Undemann. Pastor Undemann left at least two great monuments to his passion for his Lord, this Institute of Liturgical Studies and the Lutheran Book of Worship. They also left us memories of a gracious, cultured way of life controlled by an abiding love of the Church and her worship

A global Ocean Bottom Pressure data base as ground-truth reference for GRACE gravity field products

The GRACE satellite mission provides monthly estimates of the gravity field of the Earth. Differences between the monthly solutions are induced by mass redistribution on the Earth. Over the continents, the hydrological cycle represents the largest signals, which are readily observed by GRACE. Over the oceans, however, gravity field changes are about an order of magnitude smaller, close to the accuracy limits of the present GRACE solutions. Nevertheless, GRACE measurements may prove as an important tool to obtain integral estimates of water mass redistribution, sea level changes and geostrophic current variability. In order to validate and improve the gravity field products, GRACE is to be compared against ocean models and in-situ observations of Ocean Bottom Pressure (OBP). Time series of OBP sensors deployed by Alfred-Wegener-Institut in the Antarctic Circumpolar Current, as well as measurements from other locations of the global ocean are included in a OBP database that is currently under development at AWI, in close cooperation with Proudman Oceanographic Laboratory (POL, Liverpool). The mutual comparison of in-situ and ocean model data with different GRACE products provided by CSR, GFZ, GRGS, ITG and JPL will help to optimize data processing methods and corrections applied to GRACE, and to identify the performance of GRACE to detect oceanic mass flux variability in different regions of the global ocean

Cynthia and Parodies

Includes: Cynthia , by Grace Ferguson and Parodies , by Gene Smith and Grace Ferguso

GRACE REED’S SUPERIORITY OVER SAMANTHA REED IN HUNTLEY FITZPATRICK’S MY LIFE NEXT DOOR

This extended essay tries to analyze superiority complex from the character of Grace Reed in Huntley Fitzpatrick’s novel My Life Next Door. In writing this paper, the writer uses library researc that is done by reading books, articles, or any written visual documents related to the topics. While in answering questions, the writer tries to analyze intrinsic aspect and extrinsic aspect with Alfred Adler’s individual psychology theory about superiority and inferiority complex. The purpose of this study is to show the kinds of Grace Reed’s superiority over Samantha Reed, the causes on why superiority is exist in Grace Reed’s character and to the effects of Grace’s Reed superiority towards Samantha Reed. The result show that Grace Reed’s superiority can be seen from how Grace Reed behave in everyday life, the factors from the circumstances and the conflicts that happened to the character

Core Aspects of Dance: Schiller and Dewey on Grace

Part of a larger project of constructing a new, historically informed philosophy of dance, built on four phenomenological constructs that I call “Moves,” this essay concerns the third Move, “grace.” The etymology of the word “grace” reveals the entwined meanings of pleasing quality and authoritative power, which may be combined as “beautiful force.” I examine the treatments of grace in German philosopher Friedrich Schiller, who understands it as playful, naive transformation of matter; and in American philosopher John Dewey, for whom it represents rhythmic organism/environment reversal. I conclude by showing how “grace” can be used in analyzing various types of dance, which in turn suggests transformational potential for philosophy, dance, and society as a whole