Measuring evaporation across canopy phenophases of a natural forest: Miombo forest, Southern Africa
Abstract. Atmospheric water demand drives forest evaporation controlled by the plant physiological properties within available moisture storage thresholds. The pattern and magnitude of African Miombo Forest transpiration across dry season canopy phenophases are unknown. This is because estimating forest evaporation in African ecosystems continues to be a challenge as flux observation towers are scant, if not completely lacking in most ecosystems like the Miombo Forest, one of Africa’s largest woodland formations. Moreover, in the Miombo Forest, satellite data-based evaporation products (i.e., GLEAM, MOD16, SSEBop and WaPOR) show significant discrepancies in both pattern and amounts of evaporation especially during the dry season canopy phenophases. Despite the main limitations with estimation of forest evaporation the development and application of the distributed temperature sensing (DTS) system is providing deepened insights and improved accuracy in forest energy partitioning for evaporation assessment. In this study the Bowen ratio distributed temperature sensing (BR-DTS) approach is used to partition available energy and estimate evaporation across three Miombo Forest canopy phenophases covering the entire 2021 dry season and early rain season. Furthermore, four satellite evaporation products are compared to the field observations. Results show that evaporation appears to follow the net radiation and air temperature pattern with the lowest values observed during the most net radiation and air temperature depressed periods and highest values during the peak net radiation and air temperature. Evaporation continues to rise even during the driest period in the dormant leaf phenophase when canopy cover is said to be at its minimum. This is possibly facilitated by the retention of about 70 percent canopy cover during the dry season which transpires within the adapted thresholds constrained by physiological properties of each Miombo Forest species with access to ground water and vegetative water storage. This goes to show that during the dry season Miombo species may not be as water stressed as imagined. When compared to field observations all four-satellite evaporation products underestimate evaporation with only the WaPOR showing a similar pattern of evaporation during the dry season. The differences between field observations and satellite-based evaporation products can be attributed to the model structure, processes as well as inputs.
Henry Zimba et al.
Status: final response (author comments only)
RC1: 'Comment on hess-2022-303', Anonymous Referee #1, 08 Nov 2022
AC1: 'Reply on RC1', Henry Musonda Zimba, 10 Dec 2022
- AC3: 'Reply on AC1', Henry Musonda Zimba, 05 Feb 2023
- AC1: 'Reply on RC1', Henry Musonda Zimba, 10 Dec 2022
RC2: 'Comment on hess-2022-303', Anonymous Referee #2, 10 Nov 2022
AC2: 'Reply on RC2', Henry Musonda Zimba, 12 Dec 2022
- AC4: 'Reply on AC2', Henry Musonda Zimba, 05 Feb 2023
- AC2: 'Reply on RC2', Henry Musonda Zimba, 12 Dec 2022
Henry Zimba et al.
ZAMSECUR Project Miombo Forest, Zambia, Southern Africa https://doi.org/10.4121/20492934.v1
Henry Zimba et al.
Viewed (geographical distribution)
The authors present a well written manuscript on their research which describes the measurement of evaporation in a Miombo forest using the BR-DTS approach. The research has a clear aim and justification, with a throrough description of the methodological approach.
The results of the research are presented clearly and discussed adequately.
The attached PDF includes a few minor grammatical corrections, but I would suggest an additional round of language editing.