statement_idx
int64 0
8.09k
| report
stringclasses 3
values | page_num
int64 18
2.84k
| sent_num
int64 0
78
| statement
stringlengths 13
4.29k
| confidence
stringclasses 4
values | score
int64 0
3
| split
stringclasses 2
values |
|---|---|---|---|---|---|---|---|
1,500 | AR6_WGI | 1,280 | 1 | Furthermore, parts of the EAIS have lost mass in the last two decades | high | 2 | train |
1,501 | AR6_WGI | 1,280 | 2 | As stated in SROCC, snowfall and glacier flow are the largest components determining AIS mass changes, with glacier flow acceleration (dynamic thinning) on the WAIS and the Antarctic Peninsula driving total loss trends in recent decades (very high confidence), and a partial offset of the dominating dynamic-thinning losses by increased snowfall | high | 2 | train |
1,502 | AR6_WGI | 1,281 | 6 | In summary, ice-shelf thinning, mainly driven by basal melt, is widespread around the Antarctic coast and particularly strong around the WAIS | high | 2 | train |
1,503 | AR6_WGI | 1,281 | 28 | In summary, the observed evolution of the ASE glaciers is compatible with, but not unequivocally indicating an ongoing MISI | medium | 1 | train |
1,504 | AR6_WGI | 1,285 | 28 | The SROCC assessed that ice-sheet interactions with the solid Earth are not expected to substantially slow sea level rise from marine-based ice in Antarctica over the 21st century | medium | 1 | train |
1,505 | AR6_WGI | 1,285 | 32 | Grounding line stabilization by the solid Earth response may therefore occur over the 21st century in the Amundsen Sea Embayment, where most mass loss is occurring (Section 9.4.2.1), but more generally occurs over multi-centennial to millennial time scales | medium | 1 | train |
1,506 | AR6_WGI | 1,288 | 12 | In summary, it is likely that the AIS will continue to lose mass throughout this century under all emissions scenarios – that is, dynamic losses driven by ocean warming and ice-shelf disintegration will likely continue to outpace increasing snowfall | medium | 1 | train |
1,507 | AR6_WGI | 1,288 | 32 | The SR1.5 (Hoegh-Guldberg et al., 2018) assessed that a threshold for WAIS instability may be close to 1.5°C–2°C | medium | 1 | test |
1,508 | AR6_WGI | 1,289 | 9 | Overall, increased evidence and agreement on the time scales and drivers of mass loss confirm the SR1.5 assessment that a threshold for WAIS instability may be close to 1.5°C–2°C (medium confidence), and that the probability of passing a threshold is larger for 2°C warming than for 1.5°C | medium | 1 | train |
1,509 | AR6_WGI | 1,289 | 10 | New projections agree with previous studies that only part of WAIS would be lost on multi-century time scales if warming remains less than 2°C | medium | 1 | train |
1,510 | AR6_WGI | 1,289 | 12 | Under around 2°C–3°C peak warming, complete or near-complete loss of the WAIS is projected in most studies after multiple millennia, with continent-wide mass losses of around 2–5 m SLE or more; this could occur on multi-century time scales under very high basal melting (Lipscomb et al., 2021) or widespread ice-shelf loss and/or MICI | low | 0 | test |
1,511 | AR6_WGI | 1,289 | 14 | If warming exceeds around 3°C above pre-industrial, part of the EAIS (typically the Wilkes Subglacial Basin) is projected to be lost on multi-millennial time scales | low | 0 | train |
1,512 | AR6_WGI | 1,289 | 17 | The SROCC (Meredith et al., 2019; Oppenheimer et al., 2019) assessed that Antarctic mass losses could be irreversible over decades to millennia | low | 0 | train |
1,513 | AR6_WGI | 1,289 | 22 | New research therefore confirms SROCC assessment that mass loss from the AIS is irreversible on decadal to millennial time scales (low confidence) (FAQ 9.1), and suggests that reducing atmospheric CO 2 concentrations or temperatures to pre-industrial levels may not be sufficient to prevent or reverse substantial Antarctic mass losses | low | 0 | train |
1,514 | AR6_WGI | 1,291 | 15 | Including the peripheral glaciers of the ice sheets, the global glacier mass loss rate in the period 2000–2019 is very likely 266 ± 16 Gt yr –1 (4 [3 to 6] % of glacier mass in 2000) with an increase in the mass loss rate from 240 ± 9 Gt yr –1 in 2000–2009 to 290 ± 10 Gt yr –1 in 2010–2019 | high | 2 | train |
1,515 | AR6_WGI | 1,291 | 17 | In summary, new evidence published since SROCC shows that, during the decade 2010–2019, glaciers lost more mass than in any other decade since the beginning of the observational record | very high | 3 | train |
1,516 | AR6_WGI | 1,292 | 7 | For all regions with long-term observations, glacier mass in the decade 2010–2019 was the smallest since at least the beginning of the 20th century | medium | 1 | train |
1,517 | AR6_WGI | 1,292 | 12 | There is limited evidence to assess whether the Karakoram anomaly will persist in coming decades but, due to the projected increase in air temperature throughout the region, its long-term persistence is unlikely | high | 2 | train |
1,518 | AR6_WGI | 1,295 | 3 | The SROCC assessed that global glacier mass loss by 2100, relative to 2015 will be 18 [likely range 11 to 25] % for scenario RCP2.6 and 36 [likely range 26 to 47] % for RCP8.5, and that many glaciers will disappear regardless of the emissions scenario | very high | 3 | train |
1,519 | AR6_WGI | 1,295 | 6 | Glaciers will lose 29,000 [9000 to 49,000] Gt and 58,000 [28,000 to 88,000] Gt over the period 2015–2100 for RCP2.6 and RCP8.5, respectively | medium | 1 | train |
1,520 | AR6_WGI | 1,296 | 4 | In summary, both global and regional studies agree that glacier mass loss will continue in all regions, with larger mass loss for high-emissions scenarios | high | 2 | train |
1,521 | AR6_WGI | 1,296 | 19 | It is also found in high-altitude areas of mountain ranges in both hemispheres – estimated in SROCC (Hock et al., 2019b) as representing about 27–29% of the global permafrost area | medium | 1 | train |
1,522 | AR6_WGI | 1,300 | 7 | Analysis of paleoclimate records (Pederson et al., 2011; Belmecheri et al., 2016) suggests that recent snowpack reductions in western North America are exceptional on a millennial time scale | medium | 1 | train |
1,523 | AR6_WGI | 1,303 | 10 | In summary, consistent projections from all generations of global climate models, elementary process understanding and strong covariance between snow cover and temperature on several time scales make it virtually certain that future Northern Hemisphere snow cover extent and duration will continue to decrease as global climate continues to warm, and process understanding strongly suggests that this also applies to Southern Hemisphere seasonal snow cover | high | 2 | train |
1,524 | AR6_WGI | 1,303 | 18 | Based on these updated data and methods, the GMSL change over the (pre-satellite) period 1901–1990 is assessed to be 0.12 [0.07 to 0.17, very likely range] m with an average rate of 1.35 [0.78 to 1.92, very likely range] mm yr –1 | high | 2 | train |
1,525 | AR6_WGI | 1,303 | 20 | The SROCC found that four of the five available tide gauge reconstructions that extend back to at least 1902 showed a robust acceleration | high | 2 | train |
1,526 | AR6_WGI | 1,304 | 16 | For the periods 1901–1990 and 1901–2018, the assessed very likely range for the sum of components is found to be consistent with the assessed very likely range of observed GMSL change | medium | 1 | train |
1,527 | AR6_WGI | 1,304 | 19 | While the combined mass loss for Greenland and glaciers is consistent with SROCC, updates in the underlying datasets lead to differences in partitioning of the mass loss.9.6.1.2 Global Mean Sea Level Change Budget in the Satellite Era The SROCC (Oppenheimer et al., 2019) concluded that GMSL increased at a rate of 3.16 [2.79 to 3.53, very likely range] mm yr –1 in the period 1993–2015 (the satellite altimetry era), and a rate of 3.58 [3.10 to 4.06, very likely range] mm yr –1 in the period 2006–2015 – the Gravity Recovery and Climate Experiment (GRACE)/Argo data era | high | 2 | train |
1,528 | AR6_WGI | 1,304 | 20 | An updated assessment for the periods 1993–2018 and 2006–2018 yields values of 3.25 [2.88 to 3.61] and 3.69 [3.21 to 4.17] mm yr –1 | high | 2 | train |
1,529 | AR6_WGI | 1,304 | 21 | Based on the GMSL assessed time series presented in Section 2.3.3.3, GMSL acceleration is estimated as 0.075 [0.066 to 0.080] mm yr –2 for 1971–2018 and 0.094 [0.082–0.115] mm yr –2 for 1993–2018 | high | 2 | train |
1,530 | AR6_WGI | 1,304 | 26 | For both periods in the satellite era – that is, 1993–2018 and 2006–2018 – the sum of contributions is consistent with the total observed GMSL change | high | 2 | train |
1,531 | AR6_WGI | 1,304 | 31 | Because of the increased ice-sheet mass loss, the total loss of land ice (glaciers and ice sheets) was the largest contributor to GMSL rise over the period 2006–2018 | high | 2 | train |
1,532 | AR6_WGI | 1,306 | 17 | In summary, the regional sea level budget, using either observations or models, can currently only be closed on basin scales | medium | 1 | train |
1,533 | AR6_WGI | 1,307 | 14 | Adding the projected sea level change from land ice mass loss and groundwater extraction strengthens and modifies the forced signal, leading to times of emergence 10 to 20 years earlier in most parts of the ocean, except in regions close to sources of mass loss, with emergence over 50% of the ocean area by 2020, and nearly everywhere by 2100 | medium | 1 | train |
1,534 | AR6_WGI | 1,307 | 15 | In summary, detection of forced regional changes for some ocean areas in recent decades is possible | medium | 1 | train |
1,535 | AR6_WGI | 1,308 | 6 | The SROCC assessment that past multi-metre sea level changes have resulted from significant ice-sheet changes beyond those presently observed is confirmed (very high confidence).Cross-Chapter Box 9.1 (continued) The Earth system gained substantial energy over the period 1971–2018 | high | 2 | train |
1,536 | AR6_WGI | 1,308 | 7 | Ocean warming dominates the energy inventory change | high | 2 | train |
1,537 | AR6_WGI | 1,308 | 14 | A related assessment presented in Chapter 7 demonstrates closure of the global energy budget | high | 2 | train |
1,538 | AR6_WGI | 1,309 | 3 | Partly on the basis of these studies, SROCC proposed a ‘plausible’ upper bound on GMSL of 25 m | low | 0 | train |
1,539 | AR6_WGI | 1,309 | 4 | Ice-sheet model simulations indicate that Northern Hemisphere glaciation was limited to high-elevation regions in eastern and southern Greenland | medium | 1 | train |
1,540 | AR6_WGI | 1,309 | 5 | Southern Hemisphere glaciation was characterized by an Antarctic Ice Sheet (AIS) reduced in volume from the present | medium | 1 | train |
1,541 | AR6_WGI | 1,309 | 7 | In summary, under a past warming level of around 2.5°C–4°C, ice sheets in both hemispheres were reduced in extent compared to present | high | 2 | train |
1,542 | AR6_WGI | 1,309 | 8 | Proxy-based evidence (Section 2.3.3.3) combined with numerical modelling indicates that, on millennial time scales, the GMSL contribution arising from ice sheets was >5 m (high confidence) or >10 m | medium | 1 | train |
1,543 | AR6_WGI | 1,309 | 12 | The GMSL was 6–13 m above present | medium | 1 | train |
1,544 | AR6_WGI | 1,309 | 16 | In summary, geological reconstructions and numerical simulations consistently show that past warming levels of <2°C (GMST) are sufficient to trigger multi- metre mass loss from both the Greenland and Antarctic ice sheets if maintained for millennia | high | 2 | train |
1,545 | AR6_WGI | 1,309 | 21 | Since AR5, information has improved about the LIG, when GMST was about 0.5°C–1.5°C above 1850–1900 | medium | 1 | train |
1,546 | AR6_WGI | 1,309 | 24 | It is virtually certain that GMSL was higher than today, likely by 5–10 m | medium | 1 | train |
1,547 | AR6_WGI | 1,310 | 15 | Of the residual, up to about 1.4 m may be ascribed to groundwater, leaving a shortfall of 16 ± 10 m yet to be allocated among land ice reservoirs or lakes.9.6.2.5 Last Deglacial Transition: Meltwater pulse 1A During Meltwater pulse 1A (MWP-1A), GMSL very likely | medium | 1 | train |
1,548 | AR6_WGI | 1,310 | 22 | In summary, MWP-1A appears to have been driven by a combination of melt in North America (high confidence), Eurasia (low confidence), and Antarctica | low | 0 | train |
1,549 | AR6_WGI | 1,310 | 32 | At 6 ka, GMSL was –3.5 to +0.5 m | medium | 1 | train |
1,550 | AR6_WGI | 1,311 | 1 | Geochronological and numerical modelling studies indicate that it is likely | medium | 1 | train |
1,551 | AR6_WGI | 1,311 | 11 | In summary, higher-than-pre-industrial GMST during the mid-Holocene coincided with recession of the Greenland Ice Sheet to a smaller-than-present extent | high | 2 | train |
1,552 | AR6_WGI | 1,311 | 14 | In summary, both proxies and model simulations indicate that GMSL changes during the early to mid-Holocene were the result of episodic pulses, due to drainage of meltwater lakes, superimposed on a trend of steady rise due to continued ice-sheet retreat | high | 2 | train |
1,553 | AR6_WGI | 1,311 | 15 | The combination of tide gauge observations and geological reconstructions indicates that a sustained increase of GMSL began between 1820–1860 and led to a 20th-century GMSL rise that was very likely | high | 2 | train |
1,554 | AR6_WGI | 1,311 | 19 | In summary, rates of RSL rise exceeding the pre-industrial background rate of rise are apparent in parts of the North Atlantic in the 19th century (medium confidence), and in most of the world in the 20th century | high | 2 | train |
1,555 | AR6_WGI | 1,313 | 2 | Considering also projections incorporating MICI or SEJ | low | 0 | train |
1,556 | AR6_WGI | 1,316 | 21 | RSL rise associated with GRD is very likely to be largest in the Pacific, due to the combined effects of projected GrIS, AIS and glacier mass loss | high | 2 | train |
1,557 | AR6_WGI | 1,316 | 24 | In parts of north-eastern North America and north-western Europe, GRD effects associated with mass loss from southern Greenland will lead to an RSL fall, whereas mass loss from northern Greenland will lead to an RSL rise | high | 2 | train |
1,558 | AR6_WGI | 1,318 | 13 | In particular, under SSP5-8.5, low-confidence processes could lead to a total GMSL rise of 0.6–1.6 m over this time period (17th–83rd percentile range of p-box, including SEJ- and MICI-based projections), with 5th–95th percentile projections extending to 0.5–2.3 m | low | 0 | train |
1,559 | AR6_WGI | 1,319 | 5 | Approximately 60% (SSP1-1.9) to 70% (SSP5-8.5) of the global coastline has a projected median 21st century regional RSL rise within ±20% of the global mean m 1950 2000 2050 2100 2150 00.511.522.5 SSP5-8.5 SSP3-7.0 SSP2-4.5 SSP1-2.6 SSP1-1.9 HistoricalMedian (medium confidence) Likely range | medium | 1 | train |
1,560 | AR6_WGI | 1,320 | 1 | Consistent with AR5, loss of land ice mass will be an important contributor to spatial patterns in RSL change (high confidence), with ocean dynamic sea level being particularly important as a dipolar contributor in the north-west Atlantic, a positive contributor in the Arctic Ocean, and a negative contributor in the Southern Ocean south of the Antarctic Circumpolar Current | medium | 1 | train |
1,561 | AR6_WGI | 1,320 | 2 | As today, VLM will remain a major driver of RSL change | high | 2 | train |
1,562 | AR6_WGI | 1,320 | 3 | Uncertainty in RSL projections is greatest in tectonically active areas in which VLM varies over short distances (e.g., Alaska) and in areas potentially subject to large ocean dynamic sea level change (e.g., the north-western Atlantic) | high | 2 | train |
1,563 | AR6_WGI | 1,321 | 12 | The SROCC projected 0.6–1.0 m under RCP2.6 and 2.3–5.3 m under RCP8.5 | low | 0 | train |
1,564 | AR6_WGI | 1,322 | 2 | Under SSP5-8.5, GMSL will rise between 1.7 and 6.8 m by 2300 in the absence of MICI and by up to 16 m considering MICI, a wider range than AR5 or SROCC assessments, but consistent with published projections | low | 0 | train |
1,565 | AR6_WGI | 1,323 | 3 | On the basis of modelling studies, paleo constraints, single-ice-sheet studies finding multimillennial nonlinear responses from both the Greenland and Antarctic ice sheets (Sections 9.4.1.4 and 9.4.2.6), and the underlying physics, we conclude that GMSL commitment is nonlinear in peak warming on time scales of both 2,000 and 10,000 years | medium | 1 | train |
1,566 | AR6_WGI | 1,323 | 4 | Although thermosteric sea level will start to decline slowly about 2,000 years after emissions cease, the slower responses from the Greenland and Antarctic ice sheets mean that GMSL will continue to rise for 10,000 years under most scenarios | medium | 1 | train |
1,567 | AR6_WGI | 1,323 | 10 | Carbon dioxide removal, solar radiation modification, and local ice-shelf engineering may be effective at reducing the yet-to-be- realized sea level commitment, but ineffective at reversing GMSL rise | low | 0 | test |
1,568 | AR6_WGI | 1,324 | 6 | In doing so, we note upfront that the main uncertainty related to high-end sea level rise is ‘when’ rather than ‘if’ it arises: the upper limit of 1.01 m of likely sea level range by 2100 for the SSP5-8.5 scenario will be exceeded in any future warming scenario on time scales of centuries to millennia | high | 2 | train |
1,569 | AR6_WGI | 1,325 | 6 | As in AR5 and SROCC, tide gauge observations show that RSL rise (Section 9.6.1.3) is the primary driver of changes in ESWL at most locations and, across tide gauges, has led to a median 165% increase in high-tide flooding over 1995–2014 relative to those over 1960–1980 | high | 2 | train |
1,570 | AR6_WGI | 1,325 | 7 | Some locations exhibit substantial differences between long-term RSL trends and ESWL | high | 2 | train |
1,571 | AR6_WGI | 1,325 | 11 | Failing to consider the non-linear interactions between tide, surge and RSL may overestimate trends in ESWL | low | 0 | train |
1,572 | AR6_WGI | 1,326 | 3 | Combined, observations and models indicate RSL rise and direct anthropogenic factors are the primary drivers of observed tidal changes at tide gauge stations | medium | 1 | train |
1,573 | AR6_WGI | 1,326 | 17 | On the basis of satellite altimeter observations, SROCC reported increasing extreme wave heights in the Southern and North Atlantic oceans of around 1.0 and 0.8 cm yr –1, respectively, over the period 1985–2018 | medium | 1 | train |
1,574 | AR6_WGI | 1,326 | 18 | The SROCC (Collins et al., 2019) also identified sea ice loss in the Arctic as leading to increased wave heights over the period 1992–2014 | medium | 1 | train |
1,575 | AR6_WGI | 1,326 | 26 | However, sensitivity of processing techniques, inadequate spatial distribution of observations, and homogeneity issues in available records limit confidence in reported trends | medium | 1 | train |
1,576 | AR6_WGI | 1,326 | 28 | Detection and attribution of the human influence on climatic changes in surges, and waves remains a challenge (Ceres et al., 2017), with limited evidence to suggest in some instances – for example, poleward migration of tropical cyclones in the Western North Pacific (Section 11.7.1.2), changes in surges and waves can be attributed to anthropogenic climate change | low | 0 | train |
1,577 | AR6_WGI | 1,326 | 30 | The close relationship between local ESL and long-term RSL change, combined with the robust attribution of GMSL change (Section 9.6.1.4), implies that observed global changes in ESL can be attributed, at least in part, to human-caused climate change | medium | 1 | train |
1,578 | AR6_WGI | 1,328 | 8 | The SROCC showed that currently rare ESL events (e.g., with an average return period of 100 years) will occur annually or more frequently at most available locations for RCP4.5 by the end of the century | high | 2 | train |
1,579 | AR6_WGI | 1,328 | 17 | By 2100, the median frequency amplification factor is projected to be 163 for SSP1-2.6, 325 for SSP2-4.5, and 532 for SSP5-8.5, with respectively 60%, 71%, and 82% of the stations experiencing a currently 1% annual probability event at least yearly | medium | 1 | train |
1,580 | AR6_WGI | 1,328 | 28 | In summary, despite waves and surges being non-negligible contributors to projected ETWL and ECWL changes (Vousdoukas et al., 2018; Melet et al., 2020), RSL change is expected to be the main driver in changes in future ESL return periods in most areas | medium | 1 | train |
1,581 | AR6_WGI | 1,328 | 32 | At local and regional scales, anthropogenic factors such as major land reclamation efforts, as in the East China Sea (Song et al., 2013) or differing national coastal management strategies (maintaining the present coastline position or managed retreat) will locally modulate the influence of GMSL rise on tidal amplitude | medium | 1 | train |
1,582 | AR6_WGI | 1,330 | 11 | Thus, projections of ESL that do not consider correlations between and among sea level forced and atmospherically forced drivers can differ strongly from coupled projections | medium | 1 | train |
1,583 | AR6_WGI | 1,330 | 12 | The SROCC (Collins et al., 2019) highlighted compound events, or coincident occurrence of multiple hazards, as an example of deep uncertainty, and noted that failing to account for multiple factors contributing to extreme events will lead to underestimation of the probabilities of occurrence | high | 2 | train |
1,584 | AR6_WGI | 1,382 | 10 | Distilling regional climate information from multiple lines of evidence and taking the user context into account will increase the fitness, usefulness and relevance for decision-making and enhances the trust users will have in applying it | high | 2 | train |
1,585 | AR6_WGI | 1,382 | 13 | Taking the values of the relevant actors into account when co-producing climate information, and translating this information into the broader user context, improves the usefulness and uptake of this information | high | 2 | train |
1,586 | AR6_WGI | 1,382 | 15 | The availability of multiple observational records, including reanalyses, that are fit for evaluating the phenomena of interest and account for observational uncertainty, are fundamental for both understanding past regional climate change and assessing climate model performance at regional scales | high | 2 | train |
1,587 | AR6_WGI | 1,382 | 16 | Employing tailored, process-oriented and potentially multivariate diagnostics to evaluate whether a climate model realistically simulates relevant aspects of present-day regional climate increases trust in future projections of these aspects | high | 2 | train |
1,588 | AR6_WGI | 1,382 | 18 | Precipitation measurements in mountainous areas, especially of solid precipitation, are strongly affected by gauge location and setup | very high | 3 | train |
1,589 | AR6_WGI | 1,382 | 23 | Regional reanalyses represent the distributions of precipitation, surface air temperature, and surface wind, including the frequency of extremes, better than global reanalyses | high | 2 | train |
1,590 | AR6_WGI | 1,382 | 26 | Global models by themselves provide a useful line of evidence for the construction of regional climate information through the attribution or projection of forced changes or the quantification of the role of the internal variability | high | 2 | train |
1,591 | AR6_WGI | 1,382 | 27 | Dynamical downscaling using regional climate models adds value in representing many regional weather and climate phenomena, especially over regions of complex orography or with heterogeneous surface characteristics | very high | 3 | test |
1,592 | AR6_WGI | 1,382 | 28 | Increasing climate model resolution improves some aspects of model performance | high | 2 | train |
1,593 | AR6_WGI | 1,382 | 29 | Some local-scale phenomena such as land–sea breezes and mountain wind systems can only be realistically represented by simulations at a resolution of the order of 10 km or finer | high | 2 | train |
1,594 | AR6_WGI | 1,382 | 30 | Simulations at kilometre-scale resolution add value in particular to the representation of convection, sub-daily precipitation extremes (high confidence) and soil-moisture– precipitation feedbacks | medium | 1 | train |
1,595 | AR6_WGI | 1,383 | 4 | Including the relevant forcings (e.g., aerosols, land-use change and stratospheric ozone concentrations) and representing the relevant feedbacks (e.g., snow–albedo, soil-moisture–temperature, soil-moisture–precipitation) in global and regional models is a prerequisite for reproducing historical regional trends and ensuring fitness for future projections | high | 2 | train |
1,596 | AR6_WGI | 1,383 | 5 | The sign of projected regional changes of variables such as precipitation and wind speed is in some cases only simulated in a trustworthy manner if relevant regional processes are represented | medium | 1 | train |
1,597 | AR6_WGI | 1,383 | 7 | Statistical downscaling methods with carefully chosen predictors and an appropriate model structure for a given application realistically represent many statistical aspects of present-day daily temperature and precipitation | high | 2 | train |
1,598 | AR6_WGI | 1,383 | 8 | Bias adjustment has proven beneficial as an interface between climate model projections and impact modelling in many different contexts | high | 2 | train |
1,599 | AR6_WGI | 1,383 | 9 | Weather generators realistically simulate many statistical characteristics of present-day daily temperature and precipitation, such as extreme temperatures and wet- and dry-day transition probabilities | high | 2 | train |
Subsets and Splits