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UNDP Climate Change Country Profiles
Liberia C. McSweeney1, M. New1,2 and G. Lizcano1
1. School of Geography and Environment, University of Oxford. 2.Tyndall Centre for Climate Change Research
http://country-profiles.geog.ox.ac.uk
General Climate
Liberia is located in West Africa on the Atlantic coast at latitudes of 4 to 8˚C. The south of Liberia has an equatorial climate, experiencing rainfall throughout the year, but the northern regions are tropical and strongly influenced by the West African Monsoon.
Most of Liberia has one wet season between May and November. This rainfall season is largely controlled by the movement of the tropical rain belt (also known as the Inter‐Tropical Conversion Zone, ITCZ), which oscillates between the northern and southern tropics over the course of a year. When the ITCZ is in its northern position, the dominant wind direction in regions south of the ITCZ is south‐westerly, blowing moist air from the Atlantic onto the continent. This pattern is referred to as the West African Monsoon, and causes exceptionally high rainfalls on the coastline of west Africa in the wet season. Monthly rainfall in coastal Liberia in the wet season can exceed 1000mm. In the winter, the dominant wind direction is reversed, the dry and dusty ‘Harmattan’ winds blow from the Sahara desert. The southern most parts of Liberia, closest to the equator, receive rainfall throughout the year.
The seasonal rainfall in this region varies considerably on inter‐annual and inter‐decadal timescales, due in part to variations in the movements and intensity of the ITCZ, and also to variations in timing and intensity of the West African Monsoon. The most well documented cause of these variations is the El Niño Southern Oscillation (ENSO). El Niño events are associated with drier conditions in West Africa.
Temperatures in Liberia are generally higher on the coast than inland. Temperatures range from 24 to 27˚C in the dry season, and 24 to 25˚C in the wet season.
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Recent Climate Trends
Temperature
• Mean annual temperature has increased by 0.8˚C between 1960 and 2006, an average rate of 0.18˚C per decade.
• There are insufficient daily data available to determine trends in daily temperature extremes for all seasons. Available data, however, indicate that despite the observed increases in mean temperature, there is no significant increase in the frequency of ‘hot’1 days. Data do indicate significantly increasing trends in the frequency of ‘hot’ nights.
o The average number of ‘hot’ nights per year in Liberia has increased by 57 (an additional 15.7% of nights2) between 1960 and 2003.
• Available daily data do not indicate decreases in the frequency of ‘cold’3 days, but do indicate significant decreases in the annual frequency of cold nights.
o The average number of ‘cold’ nights per year has decreased by 18 (4.8% of days). This rate of decrease is most rapid in MAM when the average number of cold MAM nights has decreased by 2.7 nights per month (8.6% of MAM nights) over this period.
Precipitation
• Mean annual rainfall over Liberia has decreased since 1960, but it is difficult to determine whether this is part of a long term trend because of the variable nature of rainfall in this region. The rainfall record is punctuated by wetter and drier periods; the 60s and late 70s were particularly wet, whilst the early 70s and 80s were very dry. Rainfalls in 2005 and 2006 have been very low.
• There are insufficient daily rainfall observations available from which to determine changes in extremes indices of daily rainfall.
GCM Projections of Future Climate Temperature
• The mean annual temperature is projected to increase by 0.9 to 2.6˚C by the 2060s, and 1.4 to 4.7˚C by the 2090s. Under any one emissions scenario, the range projections from the different models spans up to 1.9˚C.
• The projected rate of warming is most rapid in the northern inland regions of western Africa than the coastal regions.
1 ‘Hot’ day or ‘hot’ night is defined by the temperature exceeded on 10% of days or nights in current climate of that region and season. 2 The increase in frequency over the 43‐year period between 1960 and 2003 is estimated based on the decadal trend quoted in the summary table. 3 ‘Cold’ days or ‘cold’ nights are defined as the temperature below which 10% of days or nights are recorded in current climate of that region or season.
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• All projections indicate substantial increases in the frequency of days and nights that are considered ‘hot’ in current climate.
o Annually, projections indicate that ‘hot’ days will occur on 24‐65% of days by the 2060s, and 29‐90% of days by the 2090s. Days considered ‘hot’ by current climate standards for their season are may increase most rapidly in JAS, but the range between model projections is large, occurring on 46‐99% of days of the season by the 2090s.
o Nights that are considered ‘hot’ for the annual climate of 1970‐99 are projected to occur on 37‐89% of nights by the 2060s and 49‐97% of nights by the 2090s. Nights that are considered hot for each season by 1970‐99 standards are projected to increase most rapidly in JAS, occurring on 58‐99% of nights in every season by the 2090s.
o Projected increases in hot days and nights are more rapid in the coastal regions of West Africa than inland.
• All projections indicate decreases in the frequency of days and nights that are considered ‘cold’ in current climate. Cold days and nights occur on less than 2% of days by the 2090s and do not occur at all by the 2090s in any projections under the highest emissions scenario (A2).
Precipitation
• Projections of mean annual rainfall averaged over the country from different models in the ensemble project a wide range of changes in precipitation for Liberia, but tend towards overall increases, particularly in JAS and OND. Rainfall in JAS is projected to change by ‐15 to +23% by the 2090s, and ‐12 to +32% in OND.
• The proportion of total annual rainfall that falls in heavy4 events tends towards increases in the ensemble projections. Seasonally, this varies between tendencies to decrease in JFM and to increases in JAS and OND.
• 1‐ and 5‐day rainfall maxima in projections all tend towards increases, particularly in JAS. The range of changes in projections from the model ensemble covers both increases and decreases in all seasons.
4 A ‘Heavy’ event is defined as a daily rainfall total which exceeds the threshold that is exceeded on 5% of rainy days in current the climate of that region and season.
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Other Regional Climate Change Information
• Model simulations of precipitation changes for the Sahelian and Guinea coast regions of Africa are strongly divergent and most models fail to reproduce realistic inter‐annual and inter‐decadal rainfall variability in the Sahel in 20th century simulations. Our understanding of the processes causing tropical rainfall is insufficient to allow a prediction of the direction of change with any certainty. The IPCC identify this as an area requiring further research to understand the variety of model responses in this region (Christensen et al., 2007).
• Model simulations show wide disagreements in projected changes in the amplitude of future El Niño events. West African climate can be strongly influenced by ENSO, thus contributing to uncertainty in climate projections for this region.
• The coastal regions of Liberia may be vulnerable to sea‐level rise. Sea‐level in this region is projected by climate models to rise by the following levels5 by the 2090s, relative to 1980‐1999 sea‐level:
o 0.13 to 0.43m under SRES B1 o 0.16 to 0.53m under SRES A1B o 0.18 to 0.56m under SRES A2
• For further information on climate projections for Africa, see Christensen et al. (2007) IPCC Working Group I Report: ‘The Physical Science Basis’, Chapter 11 (Regional Climate projections): Section 11.2 (Africa).
5 Taken from the IPCC Working group I (The Physical Science Basis): Chapter 10 (Global Climate Projections) (Meehl et al., 2007). Regional sea‐level projections are estimated by applying regional adjustments (Fig 10.32, p813) to projected global mean sea‐level rise from 14 AR4 models.
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Data Summary
Observed
Mean 1970‐99
Observed
Trend 1960‐2006
Projected changes by the
2030s Projected changes by the
2060s Projected changes by the
2090s Min Median Max Min Median Max Min Median Max
Temperature
(˚C)
(change in ˚C per decade)
Change in ˚C Change in ˚C Change in ˚C
A2 0.9 1.1 1.4 1.8 2.3 2.6 2.8 3.6 4.7 Annual 25.0 0.18* A1B 0.8 1.2 1.6 1.6 2.2 2.7 2.3 2.9 4.0
B1 0.6 1.0 1.2 0.9 1.6 1.9 1.4 1.9 2.5 A2 0.9 1.2 1.6 1.9 2.3 3.1 2.9 3.9 5.3
JFM 25.8 0.17* A1B 0.8 1.2 1.7 1.6 2.3 3.0 2.3 3.0 4.3 B1 0.6 1.0 1.2 1.1 1.6 2.1 1.4 2.0 2.7 A2 0.7 1.2 1.5 1.6 2.3 2.8 2.6 3.7 5.0
AMJ 25.5 0.16* A1B 0.8 1.4 1.8 1.7 2.2 3.0 2.2 3.0 4.8 B1 0.7 1.0 1.4 0.9 1.6 2.4 1.4 2.0 2.9 A2 0.7 1.0 1.3 1.7 2.1 2.5 2.9 3.3 4.3
JAS 23.9 0.18* A1B 0.8 1.1 1.4 1.4 2.0 2.5 2.1 2.7 3.8 B1 0.3 0.9 1.2 0.7 1.4 2.0 1.3 1.7 2.3 A2 0.8 1.1 1.5 1.8 2.3 2.7 3.0 3.7 4.8
OND 24.8 0.20* A1B 0.9 1.2 1.5 1.5 2.3 2.6 2.2 2.8 3.8 B1 0.5 1.0 1.2 0.9 1.6 1.9 1.3 1.8 2.4
Precipitation
(mm per month)
(change in mm per decade)
Change in mm per month Change in mm per month Change in mm per month
A2 ‐8 ‐1 17 ‐11 2 18 ‐20 0 19 Annual 186.4 ‐5.4* A1B ‐10 ‐1 19 ‐14 ‐1 17 ‐19 2 17
B1 ‐5 1 12 ‐7 0 17 ‐14 5 23 A2 ‐10 0 9 ‐10 0 22 ‐15 ‐6 26
JFM 61.1 ‐3.4* A1B ‐7 ‐1 10 ‐12 ‐4 18 ‐15 ‐2 17 B1 ‐7 ‐1 16 ‐11 ‐2 9 ‐10 0 17 A2 ‐27 ‐2 36 ‐41 ‐4 40 ‐50 ‐6 61
AMJ 231.9 ‐10.1* A1B ‐26 0 34 ‐39 1 48 ‐66 ‐13 39 B1 ‐22 3 29 ‐27 0 44 ‐42 ‐1 57 A2 ‐22 4 23 ‐11 10 39 ‐45 2 59
JAS 312.8 ‐4.3 A1B ‐18 6 30 ‐25 6 33 ‐53 7 49 B1 ‐16 2 48 ‐18 6 19 ‐22 8 38 A2 ‐16 ‐2 16 ‐13 3 20 ‐13 6 32
OND 138.6 ‐4.0 A1B ‐8 0 8 ‐17 0 27 ‐9 9 22 B1 ‐8 0 11 ‐11 0 17 ‐6 1 17
Precipitation (%) (mm per month)
(change in % per decade)
% Change % Change % Change
A2 ‐5 0 14 ‐7 1 13 ‐16 0 15 Annual 186.4 ‐2.9* A1B ‐7 0 12 ‐9 ‐1 8 ‐15 1 12
B1 ‐4 0 7 ‐5 0 10 ‐9 3 18 A2 ‐13 0 26 ‐21 ‐1 33 ‐30 ‐9 40
JFM 61.1 ‐5.6* A1B ‐24 ‐2 16 ‐21 ‐7 28 ‐30 ‐6 26 B1 ‐15 ‐1 25 ‐41 ‐7 14 ‐35 ‐2 26 A2 ‐18 ‐2 36 ‐28 ‐2 44 ‐38 ‐4 54
AMJ 231.9 ‐4.3* A1B ‐19 0 22 ‐29 1 23 ‐45 ‐6 32 B1 ‐14 1 19 ‐19 0 28 ‐29 0 66 A2 ‐9 2 10 ‐4 3 13 ‐15 1 23
JAS 312.8 ‐1.4 A1B ‐7 1 10 ‐9 3 12 ‐15 3 21 B1 ‐6 1 16 ‐7 2 6 ‐8 4 14 A2 ‐12 ‐1 17 ‐18 3 17 ‐10 6 32
OND 138.6 ‐2.9 A1B ‐11 0 8 ‐14 0 20 ‐12 8 18 B1 ‐10 0 9 ‐17 0 12 ‐8 1 15
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Observed
Mean 1970‐99
Observed
Trend 1960‐2006
Projected changes by the
2030s Projected changes by the 2060s Projected changes by the
2090s Min Median Max Min Median Max Min Median Max
%
Frequency
Change in frequency per decade
Future % frequency Future % frequency
Frequency of Hot Days (TX90p) A2 **** **** **** 32 43 64 46 62 90
Annual 9.6 0.36 A1B **** **** **** 29 42 65 39 56 88 B1 **** **** **** 24 33 51 29 41 67 A2 **** **** **** 47 61 81 69 84 98
JFM 9.1 (0.5) A1B **** **** **** 47 61 80 59 74 97 (DJF) B1 **** **** **** 32 43 68 43 55 84
A2 **** **** **** 38 50 82 60 76 98 AMJ 9.1 (0.41) A1B **** **** **** 36 53 84 53 71 97
(MAM) B1 **** **** **** 29 42 73 35 50 86 A2 **** **** **** 42 66 96 62 87 99
JAS **** **** A1B **** **** **** 48 69 96 55 80 99 (JJA) B1 **** **** **** 28 44 89 46 54 95
A2 **** **** **** 40 57 94 59 80 99 OND **** **** A1B **** **** **** 35 58 95 50 74 99 (SON) B1 **** **** **** 30 44 85 34 54 95
Frequency of Hot Nights (TN90p) A2 **** **** **** 50 68 89 83 88 97
Annual 12.6 3.65* A1B **** **** **** 47 66 89 69 81 96 B1 **** **** **** 37 51 79 49 62 90 A2 **** **** **** 50 68 92 68 86 96
JFM **** **** A1B **** **** **** 48 71 89 62 79 94 (DJF) B1 **** **** **** 43 54 83 49 65 92
A2 **** **** **** 67 78 94 95 99 99 AMJ 12.4 (4.31*) A1B **** **** **** 60 80 95 88 96 99
(MAM) B1 **** **** **** 44 60 85 62 77 95 A2 **** **** **** 70 91 97 92 99 99
JAS **** **** A1B **** **** **** 70 89 98 82 99 99 (JJA) B1 **** **** **** 46 71 83 58 88 94
A2 **** **** **** 53 66 91 77 87 98 OND **** **** A1B **** **** **** 56 66 91 66 88 97 (SON) B1 **** **** **** 44 60 84 48 65 91
Frequency of Cold Days (TX10p) A2 **** **** **** 0 1 2 0 0 0
Annual 10.1 0.17 A1B **** **** **** 0 0 2 0 0 0 B1 **** **** **** 0 2 3 0 1 2 A2 **** **** **** 0 0 0 0 0 1
JFM **** **** A1B **** **** **** 0 0 1 0 0 1 (DJF) B1 **** **** **** 0 1 4 0 1 1
A2 **** **** **** 0 0 2 0 0 1 AMJ 10.9 (0.39) A1B **** **** **** 0 0 3 0 0 1
(MAM) B1 **** **** **** 0 1 3 0 1 3 A2 **** **** **** 0 0 0 0 0 0
JAS **** **** A1B **** **** **** 0 0 1 0 0 0 (JJA) B1 **** **** **** 0 1 3 0 0 1
A2 **** **** **** 0 0 2 0 0 0 OND 9.7 (‐0.04) A1B **** **** **** 0 0 2 0 0 0 (SON) B1 **** **** **** 0 1 2 0 1 2
Frequency of Cold Nights (TN10p) A2 **** **** **** 0 1 2 0 0 0
Annual 9.2 ‐1.12* A1B **** **** **** 0 1 2 0 0 1 B1 **** **** **** 0 2 3 0 1 2 A2 **** **** **** 0 0 2 0 0 2
JFM 11.0 (0.31) A1B **** **** **** 0 0 3 0 0 1 (DJF) B1 **** **** **** 0 1 5 0 0 3
A2 **** **** **** 0 0 0 0 0 0 AMJ 8.0 (‐2.00*) A1B **** **** **** 0 0 0 0 0 0
(MAM) B1 **** **** **** 0 0 1 0 0 1 A2 **** **** **** 0 0 1 0 0 0
JAS **** **** A1B **** **** **** 0 0 1 0 0 0 (JJA) B1 **** **** **** 0 0 1 0 0 1
A2 **** **** **** 0 0 2 0 0 0 OND 8.8 (‐0.56) A1B **** **** **** 0 0 1 0 0 1 (SON) B1 **** **** **** 0 1 3 0 1 2
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Observed
Mean 1970‐99
Observed
Trend 1960‐2006
Projected changes by the
2030s Projected changes by the
2060s Projected changes by the
2090s Min Median Max Min Median Max Min Median Max
% total rainfall falling in Heavy Events (R95pct)
% Change in % per decade
Change in % Change in %
A2 **** **** **** ‐4 2 7 ‐3 3 9 Annual **** **** A1B **** **** **** ‐3 2 6 ‐5 3 9
B1 **** **** **** ‐3 2 7 ‐4 3 9 A2 **** **** **** ‐10 ‐1 3 ‐16 ‐4 7
JFM **** **** A1B **** **** **** ‐8 ‐2 3 ‐9 ‐3 7 (DJF) B1 **** **** **** ‐7 ‐2 4 ‐8 0 8
A2 **** **** **** ‐6 0 10 ‐9 1 10 AMJ **** **** A1B **** **** **** ‐9 0 10 ‐12 0 7
(MAM) B1 **** **** **** ‐5 2 6 ‐8 0 12 A2 **** **** **** ‐3 3 6 ‐4 2 11
JAS **** **** A1B **** **** **** ‐4 3 10 ‐6 5 15 (JJA) B1 **** **** **** ‐4 2 10 ‐3 3 17
A2 **** **** **** ‐3 2 7 ‐4 3 11 OND **** **** A1B **** **** **** ‐5 1 4 ‐3 2 10 (SON) B1 **** **** **** ‐2 0 10 ‐3 2 7
Maximum 1‐day rainfall (RX1day)
mm
Change in mm per decade
Change in mm Change in mm
A2 **** **** **** ‐3 2 24 ‐3 8 51 Annual **** **** A1B **** **** **** ‐5 3 23 ‐6 4 32
B1 **** **** **** ‐10 1 20 ‐5 2 33 A2 **** **** **** ‐1 0 2 ‐3 0 0
JFM **** **** A1B **** **** **** ‐1 0 1 ‐2 0 1 (DJF) B1 **** **** **** ‐2 0 1 ‐2 0 1
A2 **** **** **** ‐6 0 11 ‐6 1 54 AMJ **** **** A1B **** **** **** ‐5 0 21 ‐6 0 44
(MAM) B1 **** **** **** ‐4 1 13 ‐4 0 21 A2 **** **** **** ‐3 3 20 ‐2 4 18
JAS **** **** A1B **** **** **** ‐6 3 20 ‐6 2 24 (JJA) B1 **** **** **** ‐7 0 15 ‐4 1 27
A2 **** **** **** ‐3 0 11 ‐3 1 13 OND **** **** A1B **** **** **** ‐6 0 6 ‐1 0 10 (SON) B1 **** **** **** ‐3 0 8 ‐4 1 6
Maximum 5‐day Rainfall (RX5day)
mm
Change in mm per decade
Change in mm Change in mm
A2 **** **** **** ‐5 6 25 ‐7 13 61 Annual **** **** A1B **** **** **** ‐9 8 40 ‐12 8 31
B1 **** **** **** ‐18 3 32 ‐8 3 39 A2 **** **** **** ‐6 ‐1 6 ‐7 ‐2 8
JFM **** **** A1B **** **** **** ‐3 ‐1 8 ‐6 ‐2 8 (DJF) B1 **** **** **** ‐4 0 7 ‐6 0 7
A2 **** **** **** ‐8 1 13 ‐10 0 72 AMJ **** **** A1B **** **** **** ‐13 0 29 ‐18 ‐2 50
(MAM) B1 **** **** **** ‐6 0 17 ‐9 ‐1 28 A2 **** **** **** ‐5 4 28 ‐8 8 24
JAS **** **** A1B **** **** **** ‐9 3 29 ‐25 8 32 (JJA) B1 **** **** **** ‐15 3 17 ‐7 2 32
A2 **** **** **** ‐6 0 13 ‐3 0 23 OND **** **** A1B **** **** **** ‐6 0 5 ‐2 1 14 (SON) B1 **** **** **** ‐7 0 17 ‐6 3 9
* indicates trend is statistically significant at 95% confidence
**** indicates data are not available
Bracketed trend values for extremes indices indicate values for the closest seasons that data is available. See documentation.
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Figure 1: Trends in annual and seasonal mean temperature for the recent past and projected future. All values shown are anomalies, relative to the 1970-1999 meanclimate. Black curves show the mean of observed data from 1960 to 2006, Brown curves show the median (solid line) and range (shading) of model simulations ofrecent climate across an ensemble of 15 models. Coloured lines from 2006 onwards show the median (solid line) and range (shading) of the ensemble projections ofclimate under three emissions scenarios. Coloured bars on the right-hand side of the projections summarise the range of mean 2090-2100 climates simulated by the15 models for each emissions scenario.
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Figure 2: Spatial patterns of projected change in mean annual and seasonal temperature for 10-year periods in the future under the SRES A2 scenario. All values areanomalies relative to the mean climate of 1970-1999. In each grid box, the central value gives the ensemble median and the values in the upper and lower cornersgive the ensemble maximum and minimum.
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Figure 3: Trends in monthly precipitation for the recent past and projected future. All values shown are anomalies, relative to the 1970-1999 mean climate. SeeFigure 1 for details.
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Figure 4: Spatial patterns of projected change in monthly precipitation for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relativeto the mean climate of 1970-1999.See Figure 2 for details.
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Figure 5: Trends in monthly precipitation for the recent past and projected future. All values shown are percentage anomalies, relative to the 1970-1999 mean climate.See Figure 1 for details.
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Figure 6: Spatial patterns of projected change in monthly precipitation for 10-year periods in the future under the SRES A2 scenario. All values are percentageanomalies relative to the mean climate of 1970-1999.See Figure 2 for details.
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Figure 7: Trends in Hot-day frequency for the recent past and projected future. See Figure 1 for details.
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Figure 8: Spatial patterns of projected change in Hot-day frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details.
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Figure 9: Trends in hot-night frequency for the recent past and projected future. See Figure 1 for details.
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Figure 10: Spatial patterns of projected change in hot-night frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details.
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Figure 11: Trends in cold-day frequency for the recent past and projected future. See Figure 1 for details.
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Figure 12: Spatial patterns of projected change in cold-day frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details.
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Figure 13: Trends in cold-night frequency for the recent past and projected future. See Figure 1 for details.
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Figure 14: Spatial patterns of projected change in cold-night frequency for 10-year periods in the future under the SRES A2 scenario. See Figure 2 for details.
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Figure 15: Trends in the proportion of precipitation falling in ’heavy’ events for the recent past and projected future. All values shown are anomalies, relative to the1970-1999 mean climate. See Figure 1 for details.
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Figure 16: Spatial patterns of projected change in the proportion of precipitation falling in ’heavy’ events for 10-year periods in the future under the SRES A2 scenario.All values are anomalies relative to the mean climate of 1970-1999. See Figure 2 for details.
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Figure 17: Trends in maximum 1-day rainfall for the recent past and projected future. All values shown are anomalies, relative to the 1970-1999 mean climate. SeeFigure 1 for details.
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Figure 18: Spatial patterns of maximum 1-day rainfall for 10-year periods in the future under the SRES A2 scenario. All values are anomalies relative to the meanclimate of 1970-1999. See Figure 2 for details.
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Figure 19: Trends in maximum 5-day rainfall for the recent past and projected future. All values shown are anomalies, relative to the 1970-1999 mean climate. SeeFigure 1 for details.
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Figure 20: Spatial patterns of projected change in maximum 5-day rainfall for 10-year periods in the future under the SRES A2 scenario. All values are anomaliesrelative to the mean climate of 1970-1999. See Figure 2 for details.
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