Rodell-2018 cause labels predicted which GRACE water-storage trends continued in GRACE-FO 2018-2026: 4 of 12 natural-variability trends kept their sign, versus 11 of 14 human and 8 of 8 climate trends
Rodell et al. (2018) mapped 34 regional terrestrial water storage (TWS) trends in GRACE data from April 2002 to March 2016. They labelled each trend as caused by climate change, direct human impact, or natural variability. We used these labels as a forecast and tested them on independent GRACE-FO data (June 2018 to August 2026). We used CSR RL06.3 mascons and approximate region polygons, which we froze with training data only (Gt/yr agreement with Rodell Table 1: r = 0.99). The test was pre-registered. Only 4 of 12 natural-variability regions kept their trend sign (persistence slope 0.17, 95% CI -0.91 to 1.39). In contrast, 11 of 14 human regions (slope 1.89, CI 0.43 to 2.61) and 8 of 8 climate regions (slope 0.79) kept their sign. Fisher test, human versus natural: p = 0.026. The slope difference had bootstrap P = 0.045, but its CI includes zero. Trend extrapolation beat holding the 2014-16 level in 8/8 climate, 7/14 human and 3/12 natural regions. At 3-degree block scale, natural-region blocks kept their sign less often (45%) than land blocks outside all regions (64%; difference -0.18, CI -0.35 to -0.01). Individual forecasts often failed. The North China Plain depletion reversed (-1.0 to +1.5 cm/yr). NW Saudi Arabia did not slow down. The Caspian loss accelerated about 3x. Four natural regions kept significant same-sign trends. Changes in a 24-month-memory GPCP precipitation store correlated with the trend changes (Spearman 0.56 in 27 non-ice regions). The pre-registered memory-free measure was weaker (Spearman 0.21). Limitations: few regions, approximate outlines, a different data release, GIA and leakage errors that add apparent persistence, and a background restriction to |lat| <= 60 that was not pre-registered.
GRACE · GRACE-FO · terrestrial water storage · groundwater depletion · trend persistence · forecast verification · attribution · natural variability · Rodell 2018 · CSR mascons · GPCP · pre-registered test
References
7- reviews, usesdoi:10.1038/s41586-018-0123-1
Source of the 34 regions, the trend table and the cause labels that we test as forecasts.
- usesdoi:10.15781/cgq9-nh24
CSR GRACE/GRACE-FO RL06 mascon data (RL06.3 file used).
- usesdoi:10.1002/2016JB013007
CSR mascon method reference.
- usesdoi:10.3390/atmos9040138
GPCP v2.3 monthly precipitation used for the explanation check.
- Past trends of US well levels did not persist: extrapolation raised 5-10-year forecast error by 33-134% over no change, and the post-2000 decline-acceleration excess was regionally uncertain sci:sha256:7ca3c3b9fcc192ed10577330a9917185b5db4241ef384cccb2fdf033a8984dd8
Related campaign test of well-level trend persistence and extrapolation skill in the US.
- GRACE water-storage deficits and surpluses decayed at the same rate on 2,243 land cells in 2002-2026; both stayed longer after extremes than linear precipitation models predict sci:sha256:2a272ce0fcfb5955020e580c5b6f683e12039d45b8bee777b6070e417e1bbbf3
Related campaign GRACE study of deficit and surplus decay rates.
- GRACE seasonal water load gave a weak thrust-timing signal that did not replicate, and no fault-type sign contrast, in global shallow GCMT Mw 5+ mainshocks, 2002-2026 sci:sha256:7184e3ca8e705c7f1821efa1d5a15e4c4783218097677a59a269fcc8859179c1
Earlier campaign use of the same CSR mascon product.
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Related campaign test of GRACE trend persistence into GRACE-FO.