Table 1. Description of collection location of Coffea canephora study material
Location (Code) Geo- reference
Cultivation status
Cultivation status
No. of genotypes
Climatic zones
PET (mm y-1) WI PET (mm y-1) WI
Annua l mean temper ature (°C)
Annua l precipi tation (mm)
Budongo (BD) 01°43′27″N 31°32′45″E
wild
wild
16
K
1740
0.76
23
1322
Itwara (IT) 00°47′29″N 30°28′19″E
wild
wild
10
L
1604
0.89
20
1422
Kalangala (KL) 00°26′S 32°15′E
wild & feral
19
A1
1560
1.25
21
1942
Kawanda (KW) 0°24′30.42″N 32°32′09″E
cultivated
19
B
1624
0.76
22
1238
Kibale (KB) 00°30′N 30°24′ E
wild
9
L
1637
0.77
20
1267
Kituza (KT) 0°15′26.81″N 32°47′27.7″E
cultivated
28
B
1573
0.93
21
1464
Mabira (MB) 0°23′54″N 33°0′59″E
wild
15
B
1652
0.82
22
1356
Malabigambo (ML)
00°57′7′′S wild 31°38′25′′E
00°57′7′′S wild 31°38′25′′E
00°57′7′′S wild 31°38′25′′E
7
A1
1604
0.88
21
1414
Zoka (ZK) 03°01’03.0”N wild 31°39’21.0”E 03°01’03.0”N wild 31°39’21.0”E 03°01’03.0”N wild 31°39’21.0”E
25
J
1869
0.68
24
1267
Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects. Climatic zones as classified by Basalirwa (1995) A1, B, K, L, J (see Appendix Fig. A.1.); PET values were estimated following Hargreaves and Samani (1985) who use mean monthly temperature, mean monthly temperature range and mean monthly extra-terrestrial radiation (Zomer et al., 2008) while WI (wetness index; (Aridity index in (Zomer et al., (2008) ) defined as a ratio of mean annual precipitation to mean annual potential evapo-transpiration (PET). Note that genotypes from Kawanda and Kituza are not in the analysis of location effects.