Özet
Our current understanding of semiarid ecosystems is that they tend to display higher vegetation greenness on polar-facing slopes (PFS) than on equatorial-facing slopes (EFS). However, recent studies have argued that higher vegetation greenness can occur on EFS during part of the year. To assess whether this seasonal reversal of aspect-driven vegetation is a common occurrence, we conducted a global-scale analysis of vegetation greenness on a monthly time scale over an 18-year period (2000–2017). We examined the influence of climate seasonality on the normalized difference vegetation index (NDVI) values of PFS and EFS at 60 different catchments with aspect-controlled vegetation located across all continents except Antarctica. Our results show that an overwhelming majority of sites (70%) display seasonal reversal, associated with transitions from water-limited to energy-limited conditions during wet winters. These findings highlight the need to consider seasonal variations of aspect-driven vegetation patterns in ecohydrology, geomorphology, and Earth system models.
| Orijinal dil | İngilizce |
|---|---|
| Makale numarası | e2020GL088918 |
| Dergi | Geophysical Research Letters |
| Hacim | 47 |
| Basın numarası | 15 |
| DOI'lar | |
| Yayın durumu | Yayınlandı - 16 Ağu 2020 |
Bibliyografik not
Publisher Copyright:©2020. The Authors.
Finansman
We thank the editor (Valeriy Y. Ivanov), Todd Hawbaker, and three anonymous reviewers for comments and suggestions which improved the content of this paper. We thank Sandra C. Cooper for thorough and careful technical editing. O. Yetemen acknowledges support from the University of Newcastle Research Advantage for Early Career Researcher (ECR) Higher Degree by Research (HDR) scholarship and the Scientific and Technological Research Council of Turkey (TUBITAK) through Grant 118C329. P. M. Saco acknowledges support from the Australian Research Council through Grants FT140100610 and DP140104178. S. A. Johnstone was supported by the U.S. Geological Survey National Cooperative Geologic Mapping Program. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. We thank the editor (Valeriy Y. Ivanov), Todd Hawbaker, and three anonymous reviewers for comments and suggestions which improved the content of this paper. We thank Sandra C. Cooper for thorough and careful technical editing. O.?Yetemen acknowledges support from the University of Newcastle Research Advantage for Early Career Researcher (ECR) Higher Degree by Research (HDR) scholarship and the Scientific and Technological Research Council of Turkey (TUBITAK) through Grant 118C329. P.?M. Saco acknowledges support from the Australian Research Council through Grants FT140100610 and DP140104178. S.?A.?Johnstone was supported by the U.S. Geological Survey National Cooperative Geologic Mapping Program. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
| Finansörler | Finansör numarası |
|---|---|
| TUBITAK | 118C329 |
| U.S. Geological Survey National Cooperative Geologic Mapping Program | |
| U.S. Government | |
| University of Newcastle Research | |
| Australian Research Council | DP140104178, FT140100610 |
| Türkiye Bilimsel ve Teknolojik Araştirma Kurumu |