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. |